现代地质 ›› 2023, Vol. 37 ›› Issue (03): 613-626.DOI: 10.19657/j.geoscience.1000-8527.2021.053
收稿日期:
2021-04-12
修回日期:
2023-03-05
出版日期:
2023-06-10
发布日期:
2023-07-20
作者简介:
徐立明,男,硕士,助理工程师, 1989年出生,矿物学、岩石学、矿床学专业,主要从事矿床地球化学研究。Email: xlmcugb@126.com。
基金资助:
XU Liming(), LIU Tao, ZHENG Jilin
Received:
2021-04-12
Revised:
2023-03-05
Online:
2023-06-10
Published:
2023-07-20
摘要:
大兴安岭广泛出露中生代花岗岩,本文选择大兴安岭北段阿里河镇岩体进行锆石U-Pb年代学和地球化学研究,通过对比大兴安岭北段、中南段和华南等地中生代花岗岩的地球化学特征,探讨岩石成因和产出的大地构造环境。2件花岗岩样品的锆石U-Pb定年结果分别是(134.6±1.5) Ma和(134.4±1.0) Ma,表明岩石的侵入时代应为早白垩世。阿里河镇岩体主要岩石组合为二长花岗岩-正长花岗岩-碱长花岗岩,暗色矿物含量普遍较低,发育晶洞构造。野外调查可见白岗岩和细晶岩出现,且在花岗岩体边部发育伟晶岩脉。该岩体在化学组成上具有高硅(73.63%~77.81%),富碱(Na2O+K2O=7.78%~8.97%),高分异指数DI(91.71~96.80)、过铝质(A/CNK=1.01~1.11)和贫钙、镁的特征,富集大离子亲石元素Rb、Th、U和K,亏损高场强元素Nb、Ta、P和Ti。其微量元素Zr/Hf比值与Zr含量呈正相关,Nb/Ta比值与Ta含量呈负相关,上述变化特征与华南高分异花岗岩类似。综合地质和地球化学特征认为阿里河镇岩体应为高分异I型花岗岩,其动力学背景可能为与蒙古—鄂霍次克洋闭合导致的后碰撞环境有关。
中图分类号:
徐立明, 刘涛, 郑吉林. 大兴安岭北段阿里河镇早白垩世高分异花岗岩的确定及其地质意义[J]. 现代地质, 2023, 37(03): 613-626.
XU Liming, LIU Tao, ZHENG Jilin. Identification and Significance of Early Cretaceous Highly Fractionated Alihe Granites, Northern Great Xing’an Range[J]. Geoscience, 2023, 37(03): 613-626.
图1 东北地区大地构造略图((a), 据文献[26]修改)、大兴安岭北段显生宙花岗岩分布图((b), 据文献[14]修改)和研究区地质简图(c)
Fig.1 Tectonic map of NE China ((a), modified from ref.[26]), distribution of Phanerozoic granitoids in the northern Great Xing’an Range ((b), modified from ref.[14]) and geologic map of the study area (c)
图2 阿里河镇岩体显微照片 (a)二长花岗岩野外露头; (b)正长花岗岩野外露头; (c)似斑状中细粒黑云母二长花岗岩; (d)似斑状细中粒正长花岗岩;(c)图为正交光, (d)图为单偏光。Pl. 斜长石; Per.条纹长石; Q.石英; Bt.黑云母; Ap.磷灰石; Sph.榍石; Chl.绿泥石
Fig.2 Thin-section photomicrographs of the Alihe granites
测点 | Pb (10-6) | U (10-6) | Th/U | 同位素比值 | 年龄(Ma) | ||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
206Pb/ 238U | ±1σ | 207Pb/ 235U | ±1σ | 207Pb/ 206Pb | ±1σ | 206Pb/ 238U | ±1σ | 207Pb/ 235U | ±1σ | 207Pb/ 206Pb | ±1σ | ||||
Hb170248-1 | 3 | 130 | 0.87 | 0.0217 | 0.0002 | 0.1506 | 0.0093 | 0.0503 | 0.0030 | 139 | 2 | 142 | 9 | 207 | 137 |
Hb170248-2 | 3 | 107 | 0.64 | 0.0225 | 0.0002 | 0.1527 | 0.0095 | 0.0493 | 0.0033 | 143 | 2 | 144 | 9 | 163 | 154 |
Hb170248-3 | 4 | 154 | 0.73 | 0.0218 | 0.0002 | 0.1516 | 0.0062 | 0.0503 | 0.0020 | 139 | 1 | 143 | 6 | 211 | 93 |
Hb170248-4 | 4 | 160 | 0.64 | 0.0223 | 0.0002 | 0.1573 | 0.0057 | 0.0512 | 0.0018 | 142 | 1 | 148 | 5 | 252 | 83 |
Hb170248-5 | 4 | 190 | 0.56 | 0.0212 | 0.0002 | 0.1451 | 0.0109 | 0.0496 | 0.0036 | 135 | 1 | 138 | 10 | 178 | 168 |
Hb170248-6 | 3 | 129 | 0.67 | 0.0215 | 0.0002 | 0.1521 | 0.0102 | 0.0513 | 0.0034 | 137 | 1 | 144 | 10 | 256 | 154 |
Hb170248-7 | 7 | 290 | 0.61 | 0.0211 | 0.0002 | 0.1504 | 0.0047 | 0.0518 | 0.0015 | 134 | 1 | 142 | 4 | 277 | 68 |
Hb170248-8 | 8 | 343 | 0.62 | 0.0210 | 0.0002 | 0.1527 | 0.0053 | 0.0527 | 0.0018 | 134 | 1 | 144 | 5 | 318 | 79 |
Hb170248-9 | 3 | 117 | 0.70 | 0.0212 | 0.0002 | 0.1491 | 0.0146 | 0.0511 | 0.0049 | 135 | 2 | 141 | 14 | 246 | 219 |
Hb170248-10 | 7 | 290 | 0.67 | 0.0214 | 0.0002 | 0.1516 | 0.0058 | 0.0514 | 0.0019 | 137 | 1 | 143 | 5 | 257 | 85 |
Hb170248-11 | 4 | 190 | 0.69 | 0.0212 | 0.0002 | 0.1521 | 0.0045 | 0.0520 | 0.0015 | 135 | 1 | 144 | 4 | 284 | 67 |
Hb170248-12 | 5 | 241 | 0.74 | 0.0207 | 0.0002 | 0.1496 | 0.0042 | 0.0524 | 0.0014 | 132 | 1 | 142 | 4 | 302 | 61 |
Hb170248-13 | 4 | 154 | 0.63 | 0.0211 | 0.0002 | 0.1486 | 0.0062 | 0.0511 | 0.0020 | 135 | 1 | 141 | 6 | 246 | 92 |
Hb170248-14 | 7 | 286 | 0.88 | 0.0204 | 0.0002 | 0.1498 | 0.0038 | 0.0533 | 0.0013 | 130 | 1 | 142 | 4 | 343 | 55 |
Hb170248-15 | 6 | 268 | 0.47 | 0.0206 | 0.0002 | 0.1457 | 0.0048 | 0.0514 | 0.0016 | 131 | 1 | 138 | 5 | 260 | 73 |
Hb170248-16 | 1 | 49 | 0.65 | 0.0213 | 0.0003 | 0.1510 | 0.0211 | 0.0514 | 0.0069 | 136 | 2 | 143 | 20 | 259 | 308 |
Hb170248-17 | 3 | 140 | 0.64 | 0.0210 | 0.0002 | 0.1512 | 0.0074 | 0.0521 | 0.0025 | 134 | 1 | 143 | 7 | 291 | 109 |
Hb170248-18 | 5 | 223 | 0.72 | 0.0206 | 0.0002 | 0.1472 | 0.0082 | 0.0518 | 0.0028 | 132 | 1 | 139 | 8 | 276 | 124 |
Hb170248-19 | 4 | 158 | 0.57 | 0.0208 | 0.0002 | 0.1477 | 0.0063 | 0.0515 | 0.0022 | 133 | 1 | 140 | 6 | 264 | 98 |
Hb170248-20 | 6 | 275 | 0.47 | 0.0207 | 0.0002 | 0.1476 | 0.0040 | 0.0518 | 0.0013 | 132 | 1 | 140 | 4 | 277 | 59 |
Hb170248-21 | 6 | 266 | 0.49 | 0.0204 | 0.0002 | 0.1476 | 0.0053 | 0.0526 | 0.0018 | 130 | 1 | 140 | 5 | 310 | 80 |
Hb170248-22 | 5 | 240 | 0.65 | 0.0207 | 0.0002 | 0.1444 | 0.0052 | 0.0507 | 0.0018 | 132 | 1 | 137 | 5 | 226 | 82 |
Hb170248-23 | 3 | 114 | 0.56 | 0.0214 | 0.0002 | 0.1451 | 0.0087 | 0.0492 | 0.0029 | 136 | 2 | 138 | 8 | 157 | 138 |
Hb170249-1 | 6 | 214 | 1.12 | 0.0218 | 0.0002 | 0.1516 | 0.0074 | 0.0504 | 0.0025 | 139 | 1 | 143 | 7 | 212 | 114 |
Hb170249-2 | 8 | 341 | 0.64 | 0.0211 | 0.0002 | 0.1509 | 0.0039 | 0.0519 | 0.0013 | 135 | 1 | 143 | 4 | 281 | 59 |
Hb170249-3 | 9 | 374 | 0.72 | 0.0211 | 0.0002 | 0.1429 | 0.0048 | 0.0491 | 0.0016 | 135 | 2 | 136 | 5 | 152 | 79 |
Hb170249-4 | 3 | 129 | 0.52 | 0.0213 | 0.0002 | 0.1505 | 0.0103 | 0.0513 | 0.0035 | 136 | 1 | 142 | 10 | 253 | 157 |
Hb170249-5 | 7 | 275 | 0.88 | 0.0214 | 0.0002 | 0.1486 | 0.0038 | 0.0504 | 0.0012 | 137 | 1 | 141 | 4 | 212 | 57 |
Hb170249-6 | 3 | 140 | 0.99 | 0.0210 | 0.0002 | 0.1510 | 0.0082 | 0.0521 | 0.0027 | 134 | 1 | 143 | 8 | 288 | 118 |
Hb170249-7 | 5 | 200 | 1.34 | 0.0212 | 0.0002 | 0.1517 | 0.0042 | 0.0519 | 0.0014 | 135 | 1 | 143 | 4 | 283 | 62 |
Hb170249-8 | 4 | 154 | 0.87 | 0.0210 | 0.0002 | 0.1547 | 0.0057 | 0.0534 | 0.0019 | 134 | 1 | 146 | 5 | 345 | 81 |
Hb170249-9 | 6 | 123 | 0.00 | 0.0472 | 0.0005 | 0.4288 | 0.0097 | 0.0659 | 0.0014 | 297 | 3 | 362 | 8 | 802 | 43 |
Hb170249-10 | 5 | 203 | 0.66 | 0.0209 | 0.0002 | 0.1545 | 0.0073 | 0.0535 | 0.0025 | 134 | 1 | 146 | 7 | 350 | 106 |
Hb170249-11 | 2 | 88 | 1.02 | 0.0202 | 0.0002 | 0.1495 | 0.0161 | 0.0536 | 0.0057 | 129 | 2 | 141 | 15 | 354 | 239 |
Hb170249-12 | 5 | 238 | 0.54 | 0.0207 | 0.0002 | 0.1452 | 0.0043 | 0.0509 | 0.0014 | 132 | 1 | 138 | 4 | 238 | 66 |
Hb170249-13 | 3 | 134 | 0.78 | 0.0217 | 0.0002 | 0.1525 | 0.0160 | 0.0510 | 0.0052 | 138 | 2 | 144 | 15 | 240 | 233 |
Hb170249-14 | 6 | 240 | 0.52 | 0.0215 | 0.0002 | 0.1467 | 0.0058 | 0.0495 | 0.0020 | 137 | 2 | 139 | 6 | 172 | 93 |
Hb170249-15 | 4 | 184 | 0.77 | 0.0210 | 0.0002 | 0.1524 | 0.0051 | 0.0527 | 0.0017 | 134 | 1 | 144 | 5 | 315 | 72 |
Hb170249-16 | 0 | 0 | 0.00 | 0.0205 | 0.0002 | 0.1463 | 0.0048 | 0.0517 | 0.0017 | 131 | 1 | 139 | 5 | 270 | 74 |
Hb170249-17 | 2 | 92 | 0.60 | 0.0207 | 0.0002 | 0.1546 | 0.0112 | 0.0541 | 0.0040 | 132 | 1 | 146 | 11 | 376 | 167 |
Hb170249-18 | 3 | 64 | 0.00 | 0.0484 | 0.0005 | 0.3782 | 0.0152 | 0.0567 | 0.0022 | 305 | 3 | 326 | 13 | 480 | 87 |
Hb170249-19 | 3 | 119 | 0.70 | 0.0211 | 0.0002 | 0.1552 | 0.0073 | 0.0533 | 0.0024 | 135 | 2 | 147 | 7 | 344 | 101 |
Hb170249-20 | 4 | 177 | 0.61 | 0.0212 | 0.0002 | 0.1562 | 0.0058 | 0.0534 | 0.0019 | 135 | 1 | 147 | 5 | 347 | 82 |
Hb170249-21 | 6 | 266 | 1.00 | 0.0214 | 0.0002 | 0.1456 | 0.0038 | 0.0494 | 0.0013 | 136 | 1 | 138 | 4 | 167 | 59 |
Hb170249-22 | 3 | 146 | 0.59 | 0.0211 | 0.0002 | 0.1522 | 0.0081 | 0.0523 | 0.0028 | 135 | 1 | 144 | 8 | 300 | 121 |
Hb170249-23 | 3 | 114 | 0.70 | 0.0212 | 0.0002 | 0.1555 | 0.0119 | 0.0532 | 0.0040 | 135 | 1 | 147 | 11 | 339 | 171 |
Hb170249-24 | 6 | 263 | 0.86 | 0.0205 | 0.0002 | 0.1517 | 0.0070 | 0.0537 | 0.0023 | 131 | 1 | 143 | 7 | 357 | 96 |
表1 二长花岗岩(Hb170248)和正长花岗岩(Hb170249)的锆石LA-ICP-MS U-Pb定年结果
Table 1 LA-ICP-MS zircon U-Pb data of the monzonitic granite (Hb170248) and syenogranite (Hb170249)
测点 | Pb (10-6) | U (10-6) | Th/U | 同位素比值 | 年龄(Ma) | ||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
206Pb/ 238U | ±1σ | 207Pb/ 235U | ±1σ | 207Pb/ 206Pb | ±1σ | 206Pb/ 238U | ±1σ | 207Pb/ 235U | ±1σ | 207Pb/ 206Pb | ±1σ | ||||
Hb170248-1 | 3 | 130 | 0.87 | 0.0217 | 0.0002 | 0.1506 | 0.0093 | 0.0503 | 0.0030 | 139 | 2 | 142 | 9 | 207 | 137 |
Hb170248-2 | 3 | 107 | 0.64 | 0.0225 | 0.0002 | 0.1527 | 0.0095 | 0.0493 | 0.0033 | 143 | 2 | 144 | 9 | 163 | 154 |
Hb170248-3 | 4 | 154 | 0.73 | 0.0218 | 0.0002 | 0.1516 | 0.0062 | 0.0503 | 0.0020 | 139 | 1 | 143 | 6 | 211 | 93 |
Hb170248-4 | 4 | 160 | 0.64 | 0.0223 | 0.0002 | 0.1573 | 0.0057 | 0.0512 | 0.0018 | 142 | 1 | 148 | 5 | 252 | 83 |
Hb170248-5 | 4 | 190 | 0.56 | 0.0212 | 0.0002 | 0.1451 | 0.0109 | 0.0496 | 0.0036 | 135 | 1 | 138 | 10 | 178 | 168 |
Hb170248-6 | 3 | 129 | 0.67 | 0.0215 | 0.0002 | 0.1521 | 0.0102 | 0.0513 | 0.0034 | 137 | 1 | 144 | 10 | 256 | 154 |
Hb170248-7 | 7 | 290 | 0.61 | 0.0211 | 0.0002 | 0.1504 | 0.0047 | 0.0518 | 0.0015 | 134 | 1 | 142 | 4 | 277 | 68 |
Hb170248-8 | 8 | 343 | 0.62 | 0.0210 | 0.0002 | 0.1527 | 0.0053 | 0.0527 | 0.0018 | 134 | 1 | 144 | 5 | 318 | 79 |
Hb170248-9 | 3 | 117 | 0.70 | 0.0212 | 0.0002 | 0.1491 | 0.0146 | 0.0511 | 0.0049 | 135 | 2 | 141 | 14 | 246 | 219 |
Hb170248-10 | 7 | 290 | 0.67 | 0.0214 | 0.0002 | 0.1516 | 0.0058 | 0.0514 | 0.0019 | 137 | 1 | 143 | 5 | 257 | 85 |
Hb170248-11 | 4 | 190 | 0.69 | 0.0212 | 0.0002 | 0.1521 | 0.0045 | 0.0520 | 0.0015 | 135 | 1 | 144 | 4 | 284 | 67 |
Hb170248-12 | 5 | 241 | 0.74 | 0.0207 | 0.0002 | 0.1496 | 0.0042 | 0.0524 | 0.0014 | 132 | 1 | 142 | 4 | 302 | 61 |
Hb170248-13 | 4 | 154 | 0.63 | 0.0211 | 0.0002 | 0.1486 | 0.0062 | 0.0511 | 0.0020 | 135 | 1 | 141 | 6 | 246 | 92 |
Hb170248-14 | 7 | 286 | 0.88 | 0.0204 | 0.0002 | 0.1498 | 0.0038 | 0.0533 | 0.0013 | 130 | 1 | 142 | 4 | 343 | 55 |
Hb170248-15 | 6 | 268 | 0.47 | 0.0206 | 0.0002 | 0.1457 | 0.0048 | 0.0514 | 0.0016 | 131 | 1 | 138 | 5 | 260 | 73 |
Hb170248-16 | 1 | 49 | 0.65 | 0.0213 | 0.0003 | 0.1510 | 0.0211 | 0.0514 | 0.0069 | 136 | 2 | 143 | 20 | 259 | 308 |
Hb170248-17 | 3 | 140 | 0.64 | 0.0210 | 0.0002 | 0.1512 | 0.0074 | 0.0521 | 0.0025 | 134 | 1 | 143 | 7 | 291 | 109 |
Hb170248-18 | 5 | 223 | 0.72 | 0.0206 | 0.0002 | 0.1472 | 0.0082 | 0.0518 | 0.0028 | 132 | 1 | 139 | 8 | 276 | 124 |
Hb170248-19 | 4 | 158 | 0.57 | 0.0208 | 0.0002 | 0.1477 | 0.0063 | 0.0515 | 0.0022 | 133 | 1 | 140 | 6 | 264 | 98 |
Hb170248-20 | 6 | 275 | 0.47 | 0.0207 | 0.0002 | 0.1476 | 0.0040 | 0.0518 | 0.0013 | 132 | 1 | 140 | 4 | 277 | 59 |
Hb170248-21 | 6 | 266 | 0.49 | 0.0204 | 0.0002 | 0.1476 | 0.0053 | 0.0526 | 0.0018 | 130 | 1 | 140 | 5 | 310 | 80 |
Hb170248-22 | 5 | 240 | 0.65 | 0.0207 | 0.0002 | 0.1444 | 0.0052 | 0.0507 | 0.0018 | 132 | 1 | 137 | 5 | 226 | 82 |
Hb170248-23 | 3 | 114 | 0.56 | 0.0214 | 0.0002 | 0.1451 | 0.0087 | 0.0492 | 0.0029 | 136 | 2 | 138 | 8 | 157 | 138 |
Hb170249-1 | 6 | 214 | 1.12 | 0.0218 | 0.0002 | 0.1516 | 0.0074 | 0.0504 | 0.0025 | 139 | 1 | 143 | 7 | 212 | 114 |
Hb170249-2 | 8 | 341 | 0.64 | 0.0211 | 0.0002 | 0.1509 | 0.0039 | 0.0519 | 0.0013 | 135 | 1 | 143 | 4 | 281 | 59 |
Hb170249-3 | 9 | 374 | 0.72 | 0.0211 | 0.0002 | 0.1429 | 0.0048 | 0.0491 | 0.0016 | 135 | 2 | 136 | 5 | 152 | 79 |
Hb170249-4 | 3 | 129 | 0.52 | 0.0213 | 0.0002 | 0.1505 | 0.0103 | 0.0513 | 0.0035 | 136 | 1 | 142 | 10 | 253 | 157 |
Hb170249-5 | 7 | 275 | 0.88 | 0.0214 | 0.0002 | 0.1486 | 0.0038 | 0.0504 | 0.0012 | 137 | 1 | 141 | 4 | 212 | 57 |
Hb170249-6 | 3 | 140 | 0.99 | 0.0210 | 0.0002 | 0.1510 | 0.0082 | 0.0521 | 0.0027 | 134 | 1 | 143 | 8 | 288 | 118 |
Hb170249-7 | 5 | 200 | 1.34 | 0.0212 | 0.0002 | 0.1517 | 0.0042 | 0.0519 | 0.0014 | 135 | 1 | 143 | 4 | 283 | 62 |
Hb170249-8 | 4 | 154 | 0.87 | 0.0210 | 0.0002 | 0.1547 | 0.0057 | 0.0534 | 0.0019 | 134 | 1 | 146 | 5 | 345 | 81 |
Hb170249-9 | 6 | 123 | 0.00 | 0.0472 | 0.0005 | 0.4288 | 0.0097 | 0.0659 | 0.0014 | 297 | 3 | 362 | 8 | 802 | 43 |
Hb170249-10 | 5 | 203 | 0.66 | 0.0209 | 0.0002 | 0.1545 | 0.0073 | 0.0535 | 0.0025 | 134 | 1 | 146 | 7 | 350 | 106 |
Hb170249-11 | 2 | 88 | 1.02 | 0.0202 | 0.0002 | 0.1495 | 0.0161 | 0.0536 | 0.0057 | 129 | 2 | 141 | 15 | 354 | 239 |
Hb170249-12 | 5 | 238 | 0.54 | 0.0207 | 0.0002 | 0.1452 | 0.0043 | 0.0509 | 0.0014 | 132 | 1 | 138 | 4 | 238 | 66 |
Hb170249-13 | 3 | 134 | 0.78 | 0.0217 | 0.0002 | 0.1525 | 0.0160 | 0.0510 | 0.0052 | 138 | 2 | 144 | 15 | 240 | 233 |
Hb170249-14 | 6 | 240 | 0.52 | 0.0215 | 0.0002 | 0.1467 | 0.0058 | 0.0495 | 0.0020 | 137 | 2 | 139 | 6 | 172 | 93 |
Hb170249-15 | 4 | 184 | 0.77 | 0.0210 | 0.0002 | 0.1524 | 0.0051 | 0.0527 | 0.0017 | 134 | 1 | 144 | 5 | 315 | 72 |
Hb170249-16 | 0 | 0 | 0.00 | 0.0205 | 0.0002 | 0.1463 | 0.0048 | 0.0517 | 0.0017 | 131 | 1 | 139 | 5 | 270 | 74 |
Hb170249-17 | 2 | 92 | 0.60 | 0.0207 | 0.0002 | 0.1546 | 0.0112 | 0.0541 | 0.0040 | 132 | 1 | 146 | 11 | 376 | 167 |
Hb170249-18 | 3 | 64 | 0.00 | 0.0484 | 0.0005 | 0.3782 | 0.0152 | 0.0567 | 0.0022 | 305 | 3 | 326 | 13 | 480 | 87 |
Hb170249-19 | 3 | 119 | 0.70 | 0.0211 | 0.0002 | 0.1552 | 0.0073 | 0.0533 | 0.0024 | 135 | 2 | 147 | 7 | 344 | 101 |
Hb170249-20 | 4 | 177 | 0.61 | 0.0212 | 0.0002 | 0.1562 | 0.0058 | 0.0534 | 0.0019 | 135 | 1 | 147 | 5 | 347 | 82 |
Hb170249-21 | 6 | 266 | 1.00 | 0.0214 | 0.0002 | 0.1456 | 0.0038 | 0.0494 | 0.0013 | 136 | 1 | 138 | 4 | 167 | 59 |
Hb170249-22 | 3 | 146 | 0.59 | 0.0211 | 0.0002 | 0.1522 | 0.0081 | 0.0523 | 0.0028 | 135 | 1 | 144 | 8 | 300 | 121 |
Hb170249-23 | 3 | 114 | 0.70 | 0.0212 | 0.0002 | 0.1555 | 0.0119 | 0.0532 | 0.0040 | 135 | 1 | 147 | 11 | 339 | 171 |
Hb170249-24 | 6 | 263 | 0.86 | 0.0205 | 0.0002 | 0.1517 | 0.0070 | 0.0537 | 0.0023 | 131 | 1 | 143 | 7 | 357 | 96 |
样品号 | Hb170230 | Hb170246 | Hb170249 | Hb170264 | WJE078 | Hb170234 | Hb170263 | Hb170229 | Hb170248 | Hb170265 | ||
---|---|---|---|---|---|---|---|---|---|---|---|---|
岩性 | 中粗粒黑 云母正长 花岗岩 | 似斑状细 中粒正长 花岗岩 | 细中粒正 长花岗岩 | 中细粒正 长花岗岩 | 似斑状细 粒碱长花 岗岩 | 似斑状中细 粒黑云母二 长花岗岩 | 中粗粒 花岗岩 | 似斑状细 中粒二长 花岗岩 | 细中粒黑 云母二长 花岗岩 | 细中粒二 长花岗岩 | ||
SiO2 | 76.22 | 73.63 | 75.60 | 77.81 | 74.58 | 74.41 | 74.11 | 74.09 | 75.45 | 76.70 | ||
Al2O3 | 12.66 | 14.03 | 13.25 | 12.26 | 13.54 | 13.64 | 13.80 | 13.90 | 13.29 | 12.71 | ||
TiO2 | 0.21 | 0.21 | 0.13 | 0.10 | 0.19 | 0.22 | 0.22 | 0.23 | 0.13 | 0.12 | ||
Fe2O3 | 0.83 | 0.85 | 0.58 | 0.41 | 0.88 | 0.89 | 0.87 | 0.78 | 0.59 | 0.50 | ||
FeO | 0.42 | 0.42 | 0.33 | 0.19 | 0.45 | 0.49 | 0.44 | 0.53 | 0.30 | 0.29 | ||
CaO | 0.80 | 0.88 | 0.36 | 0.38 | 0.36 | 0.98 | 0.76 | 1.02 | 0.59 | 0.54 | ||
MgO | 0.40 | 0.38 | 0.22 | 0.14 | 0.40 | 0.49 | 0.37 | 0.45 | 0.24 | 0.21 | ||
K2O | 3.58 | 4.31 | 4.45 | 4.22 | 4.36 | 3.55 | 4.25 | 3.92 | 4.41 | 4.15 | ||
Na2O | 4.20 | 4.55 | 4.53 | 4.12 | 4.11 | 4.61 | 4.38 | 4.39 | 4.44 | 4.30 | ||
MnO | 0.053 | 0.064 | 0.071 | 0.051 | 0.060 | 0.060 | 0.046 | 0.034 | 0.067 | 0.056 | ||
P2O5 | 0.058 | 0.057 | 0.031 | 0.018 | 0.070 | 0.068 | 0.062 | 0.069 | 0.036 | 0.041 | ||
H2O+ | 0.36 | 0.30 | 0.24 | 0.14 | 0.63 | 0.37 | 0.45 | 0.31 | 0.15 | 0.14 | ||
H2O- | 0.22 | 0.16 | 0.17 | 0.17 | 0.41 | 0.18 | 0.24 | 0.30 | 0.16 | 0.16 | ||
烧失量 | 0.47 | 0.51 | 0.36 | 0.24 | 0.87 | 0.47 | 0.55 | 0.45 | 0.36 | 0.30 | ||
总量 | 99.91 | 99.89 | 99.92 | 99.94 | 99.87 | 99.89 | 99.88 | 99.87 | 99.91 | 99.92 | ||
Mg# | 37.97 | 36.62 | 32.16 | 31.36 | 36.51 | 40.48 | 35.28 | 39.60 | 33.91 | 34.29 | ||
DI | 93.16 | 92.92 | 96.21 | 96.80 | 94.33 | 91.90 | 93.17 | 91.71 | 95.30 | 95.73 | ||
A/CNK | 1.03 | 1.02 | 1.02 | 1.02 | 1.11 | 1.03 | 1.04 | 1.04 | 1.01 | 1.01 | ||
A/NK | 1.17 | 1.15 | 1.08 | 1.08 | 1.18 | 1.19 | 1.17 | 1.21 | 1.10 | 1.10 | ||
σ | 1.82 | 2.56 | 2.47 | 2.00 | 2.27 | 2.12 | 2.39 | 2.22 | 2.42 | 2.12 | ||
K2O/Na2O | 0.85 | 0.95 | 0.98 | 1.02 | 1.06 | 0.77 | 0.97 | 0.89 | 0.99 | 0.97 | ||
FeOT/MgO | 2.94 | 3.12 | 3.80 | 3.94 | 3.13 | 2.65 | 3.30 | 2.75 | 3.51 | 3.45 | ||
K2O+Na2O | 7.78 | 8.86 | 8.97 | 8.34 | 8.47 | 8.17 | 8.63 | 8.31 | 8.85 | 8.46 | ||
(K2O+Na2O) /CaO | 9.70 | 10.03 | 24.64 | 22.08 | 23.69 | 8.35 | 11.33 | 8.11 | 15.12 | 15.80 | ||
Sc | 1.51 | 2.25 | 2.03 | 1.01 | 1.57 | 2.04 | 1.23 | 1.18 | 1.14 | 1.13 | ||
V | 11.90 | 12.60 | 5.78 | 2.37 | 12.40 | 15.10 | 12.30 | 15.30 | 5.27 | 4.02 | ||
Cr | 2.80 | 2.41 | 1.52 | 1.69 | 4.29 | 4.20 | 1.65 | 4.63 | 1.86 | 2.25 | ||
Co | 1.61 | 2.13 | 0.79 | 0.38 | 2.99 | 2.42 | 1.80 | 2.10 | 0.76 | 0.77 | ||
Ni | 0.77 | 1.58 | 0.33 | 0.58 | 2.41 | 2.79 | 0.62 | 2.35 | 0.66 | 0.77 | ||
Ga | 16.7 | 18.3 | 17.7 | 13.7 | 14.9 | 16.6 | 17.7 | 18.0 | 16.6 | 14.9 | ||
Rb | 100 | 138 | 117 | 112 | 108 | 112 | 108 | 128 | 114 | 104 | ||
Sr | 198.0 | 241.0 | 102.0 | 47.9 | 214.0 | 273.0 | 193.0 | 345.0 | 105.0 | 87.1 | ||
Zr | 73.7 | 67.5 | 80.5 | 99.5 | 85.7 | 72.3 | 102.0 | 91.0 | 62.5 | 79.0 | ||
Nb | 10.20 | 12.30 | 13.20 | 13.00 | 9.64 | 10.20 | 10.40 | 8.86 | 12.30 | 11.20 | ||
Cs | 2.17 | 2.55 | 2.38 | 2.21 | 2.53 | 3.84 | 2.43 | 4.08 | 2.43 | 2.61 | ||
Ba | 452 | 522 | 386 | 223 | 591 | 445 | 648 | 586 | 472 | 314 | ||
Hf | 2.54 | 3.10 | 3.39 | 4.18 | 3.14 | 3.02 | 3.51 | 3.49 | 2.95 | 2.92 | ||
Ta | 0.82 | 0.98 | 0.83 | 0.94 | 0.85 | 0.88 | 0.78 | 0.72 | 0.89 | 0.75 | ||
Pb | 22.4 | 28.1 | 26.8 | 26.3 | 16.7 | 27.0 | 20.7 | 27.6 | 28.0 | 24.0 | ||
Th | 15.70 | 15.90 | 11.80 | 8.60 | 10.20 | 15.10 | 10.30 | 15.50 | 8.91 | 7.60 | ||
U | 1.94 | 2.52 | 2.50 | 2.66 | 1.71 | 2.27 | 2.53 | 3.09 | 2.65 | 1.71 | ||
Y | 10.20 | 9.39 | 13.80 | 7.63 | 6.49 | 7.00 | 12.40 | 4.25 | 13.50 | 11.50 | ||
La | 37.1 | 29.1 | 22.9 | 13.6 | 17.3 | 21.4 | 22.8 | 19.3 | 19.2 | 16.8 | ||
Ce | 56.9 | 45.9 | 44.4 | 31.3 | 33.0 | 36.1 | 46.3 | 36.9 | 38.6 | 32.7 | ||
Pr | 5.67 | 4.71 | 5.23 | 3.12 | 3.49 | 3.98 | 5.57 | 2.71 | 4.76 | 4.06 | ||
Nd | 17.4 | 14.3 | 16.8 | 10.1 | 11.7 | 12.5 | 18.5 | 8.3 | 16.1 | 13.7 | ||
Sm | 2.75 | 2.29 | 3.05 | 1.81 | 1.74 | 2.07 | 3.10 | 1.27 | 3.09 | 2.50 | ||
Eu | 0.56 | 0.53 | 0.45 | 0.26 | 0.44 | 0.54 | 0.63 | 0.47 | 0.55 | 0.40 | ||
Gd | 2.38 | 1.89 | 2.38 | 1.51 | 1.61 | 1.67 | 2.42 | 1.16 | 2.43 | 1.93 | ||
Tb | 0.33 | 0.28 | 0.39 | 0.23 | 0.22 | 0.23 | 0.36 | 0.15 | 0.41 | 0.31 | ||
Dy | 1.68 | 1.42 | 2.15 | 1.34 | 1.18 | 1.16 | 1.93 | 0.73 | 2.39 | 1.75 | ||
Ho | 0.31 | 0.27 | 0.41 | 0.26 | 0.22 | 0.21 | 0.36 | 0.14 | 0.43 | 0.34 | ||
Er | 0.98 | 0.90 | 1.29 | 0.81 | 0.68 | 0.70 | 1.11 | 0.43 | 1.36 | 1.02 | ||
Tm | 0.18 | 0.17 | 0.23 | 0.15 | 0.13 | 0.13 | 0.20 | 0.08 | 0.25 | 0.18 | ||
Yb | 1.19 | 1.24 | 1.56 | 0.93 | 0.92 | 0.94 | 1.32 | 0.60 | 1.53 | 1.14 | ||
Lu | 0.19 | 0.22 | 0.25 | 0.15 | 0.14 | 0.17 | 0.21 | 0.11 | 0.25 | 0.17 | ||
Zr/Hf | 23.90 | 29.00 | 11.34 | 21.17 | 27.10 | 28.99 | 21.75 | 23.75 | 23.77 | 27.30 | ||
Nb/Ta | 11.60 | 13.28 | 74.63 | 13.75 | 14.84 | 12.39 | 12.54 | 15.89 | 13.80 | 11.31 | ||
Rb/Sr | 0.41 | 0.56 | 0.26 | 1.08 | 1.19 | 0.51 | 0.58 | 1.15 | 2.34 | 0.50 | ||
10000Ga/Al | 2.49 | 2.47 | 2.52 | 2.11 | 2.08 | 2.30 | 2.42 | 2.45 | 2.35 | 2.21 | ||
(La/Yb)N | 21.07 | 15.89 | 9.91 | 9.82 | 12.75 | 15.31 | 11.68 | 21.79 | 8.48 | 9.96 | ||
δEu | 0.66 | 0.78 | 0.51 | 0.48 | 0.80 | 0.89 | 0.70 | 1.18 | 0.62 | 0.55 | ||
Kfs | 48 | 50 | 52 | 52 | 70 | 35 | 45 | 40 | 40 | 42 | ||
Pl | 20 | 20 | 22 | 18 | 3 | 30 | 25 | 32 | 32 | 30 | ||
Q | 27 | 26 | 22 | 28 | 27 | 30 | 28 | 25 | 23 | 25 | ||
Bt | 5 | 4 | 2 | 2 | <1 | 5 | 2 | 3 | 5 | 3 |
表2 阿里河镇岩体的主量元素(%)、微量元素(10-6)和主要矿物含量(%)
Table 2 Whole-rock major(%) and trace(10-6) elements and major mineral contents (%) of the Alihe granites
样品号 | Hb170230 | Hb170246 | Hb170249 | Hb170264 | WJE078 | Hb170234 | Hb170263 | Hb170229 | Hb170248 | Hb170265 | ||
---|---|---|---|---|---|---|---|---|---|---|---|---|
岩性 | 中粗粒黑 云母正长 花岗岩 | 似斑状细 中粒正长 花岗岩 | 细中粒正 长花岗岩 | 中细粒正 长花岗岩 | 似斑状细 粒碱长花 岗岩 | 似斑状中细 粒黑云母二 长花岗岩 | 中粗粒 花岗岩 | 似斑状细 中粒二长 花岗岩 | 细中粒黑 云母二长 花岗岩 | 细中粒二 长花岗岩 | ||
SiO2 | 76.22 | 73.63 | 75.60 | 77.81 | 74.58 | 74.41 | 74.11 | 74.09 | 75.45 | 76.70 | ||
Al2O3 | 12.66 | 14.03 | 13.25 | 12.26 | 13.54 | 13.64 | 13.80 | 13.90 | 13.29 | 12.71 | ||
TiO2 | 0.21 | 0.21 | 0.13 | 0.10 | 0.19 | 0.22 | 0.22 | 0.23 | 0.13 | 0.12 | ||
Fe2O3 | 0.83 | 0.85 | 0.58 | 0.41 | 0.88 | 0.89 | 0.87 | 0.78 | 0.59 | 0.50 | ||
FeO | 0.42 | 0.42 | 0.33 | 0.19 | 0.45 | 0.49 | 0.44 | 0.53 | 0.30 | 0.29 | ||
CaO | 0.80 | 0.88 | 0.36 | 0.38 | 0.36 | 0.98 | 0.76 | 1.02 | 0.59 | 0.54 | ||
MgO | 0.40 | 0.38 | 0.22 | 0.14 | 0.40 | 0.49 | 0.37 | 0.45 | 0.24 | 0.21 | ||
K2O | 3.58 | 4.31 | 4.45 | 4.22 | 4.36 | 3.55 | 4.25 | 3.92 | 4.41 | 4.15 | ||
Na2O | 4.20 | 4.55 | 4.53 | 4.12 | 4.11 | 4.61 | 4.38 | 4.39 | 4.44 | 4.30 | ||
MnO | 0.053 | 0.064 | 0.071 | 0.051 | 0.060 | 0.060 | 0.046 | 0.034 | 0.067 | 0.056 | ||
P2O5 | 0.058 | 0.057 | 0.031 | 0.018 | 0.070 | 0.068 | 0.062 | 0.069 | 0.036 | 0.041 | ||
H2O+ | 0.36 | 0.30 | 0.24 | 0.14 | 0.63 | 0.37 | 0.45 | 0.31 | 0.15 | 0.14 | ||
H2O- | 0.22 | 0.16 | 0.17 | 0.17 | 0.41 | 0.18 | 0.24 | 0.30 | 0.16 | 0.16 | ||
烧失量 | 0.47 | 0.51 | 0.36 | 0.24 | 0.87 | 0.47 | 0.55 | 0.45 | 0.36 | 0.30 | ||
总量 | 99.91 | 99.89 | 99.92 | 99.94 | 99.87 | 99.89 | 99.88 | 99.87 | 99.91 | 99.92 | ||
Mg# | 37.97 | 36.62 | 32.16 | 31.36 | 36.51 | 40.48 | 35.28 | 39.60 | 33.91 | 34.29 | ||
DI | 93.16 | 92.92 | 96.21 | 96.80 | 94.33 | 91.90 | 93.17 | 91.71 | 95.30 | 95.73 | ||
A/CNK | 1.03 | 1.02 | 1.02 | 1.02 | 1.11 | 1.03 | 1.04 | 1.04 | 1.01 | 1.01 | ||
A/NK | 1.17 | 1.15 | 1.08 | 1.08 | 1.18 | 1.19 | 1.17 | 1.21 | 1.10 | 1.10 | ||
σ | 1.82 | 2.56 | 2.47 | 2.00 | 2.27 | 2.12 | 2.39 | 2.22 | 2.42 | 2.12 | ||
K2O/Na2O | 0.85 | 0.95 | 0.98 | 1.02 | 1.06 | 0.77 | 0.97 | 0.89 | 0.99 | 0.97 | ||
FeOT/MgO | 2.94 | 3.12 | 3.80 | 3.94 | 3.13 | 2.65 | 3.30 | 2.75 | 3.51 | 3.45 | ||
K2O+Na2O | 7.78 | 8.86 | 8.97 | 8.34 | 8.47 | 8.17 | 8.63 | 8.31 | 8.85 | 8.46 | ||
(K2O+Na2O) /CaO | 9.70 | 10.03 | 24.64 | 22.08 | 23.69 | 8.35 | 11.33 | 8.11 | 15.12 | 15.80 | ||
Sc | 1.51 | 2.25 | 2.03 | 1.01 | 1.57 | 2.04 | 1.23 | 1.18 | 1.14 | 1.13 | ||
V | 11.90 | 12.60 | 5.78 | 2.37 | 12.40 | 15.10 | 12.30 | 15.30 | 5.27 | 4.02 | ||
Cr | 2.80 | 2.41 | 1.52 | 1.69 | 4.29 | 4.20 | 1.65 | 4.63 | 1.86 | 2.25 | ||
Co | 1.61 | 2.13 | 0.79 | 0.38 | 2.99 | 2.42 | 1.80 | 2.10 | 0.76 | 0.77 | ||
Ni | 0.77 | 1.58 | 0.33 | 0.58 | 2.41 | 2.79 | 0.62 | 2.35 | 0.66 | 0.77 | ||
Ga | 16.7 | 18.3 | 17.7 | 13.7 | 14.9 | 16.6 | 17.7 | 18.0 | 16.6 | 14.9 | ||
Rb | 100 | 138 | 117 | 112 | 108 | 112 | 108 | 128 | 114 | 104 | ||
Sr | 198.0 | 241.0 | 102.0 | 47.9 | 214.0 | 273.0 | 193.0 | 345.0 | 105.0 | 87.1 | ||
Zr | 73.7 | 67.5 | 80.5 | 99.5 | 85.7 | 72.3 | 102.0 | 91.0 | 62.5 | 79.0 | ||
Nb | 10.20 | 12.30 | 13.20 | 13.00 | 9.64 | 10.20 | 10.40 | 8.86 | 12.30 | 11.20 | ||
Cs | 2.17 | 2.55 | 2.38 | 2.21 | 2.53 | 3.84 | 2.43 | 4.08 | 2.43 | 2.61 | ||
Ba | 452 | 522 | 386 | 223 | 591 | 445 | 648 | 586 | 472 | 314 | ||
Hf | 2.54 | 3.10 | 3.39 | 4.18 | 3.14 | 3.02 | 3.51 | 3.49 | 2.95 | 2.92 | ||
Ta | 0.82 | 0.98 | 0.83 | 0.94 | 0.85 | 0.88 | 0.78 | 0.72 | 0.89 | 0.75 | ||
Pb | 22.4 | 28.1 | 26.8 | 26.3 | 16.7 | 27.0 | 20.7 | 27.6 | 28.0 | 24.0 | ||
Th | 15.70 | 15.90 | 11.80 | 8.60 | 10.20 | 15.10 | 10.30 | 15.50 | 8.91 | 7.60 | ||
U | 1.94 | 2.52 | 2.50 | 2.66 | 1.71 | 2.27 | 2.53 | 3.09 | 2.65 | 1.71 | ||
Y | 10.20 | 9.39 | 13.80 | 7.63 | 6.49 | 7.00 | 12.40 | 4.25 | 13.50 | 11.50 | ||
La | 37.1 | 29.1 | 22.9 | 13.6 | 17.3 | 21.4 | 22.8 | 19.3 | 19.2 | 16.8 | ||
Ce | 56.9 | 45.9 | 44.4 | 31.3 | 33.0 | 36.1 | 46.3 | 36.9 | 38.6 | 32.7 | ||
Pr | 5.67 | 4.71 | 5.23 | 3.12 | 3.49 | 3.98 | 5.57 | 2.71 | 4.76 | 4.06 | ||
Nd | 17.4 | 14.3 | 16.8 | 10.1 | 11.7 | 12.5 | 18.5 | 8.3 | 16.1 | 13.7 | ||
Sm | 2.75 | 2.29 | 3.05 | 1.81 | 1.74 | 2.07 | 3.10 | 1.27 | 3.09 | 2.50 | ||
Eu | 0.56 | 0.53 | 0.45 | 0.26 | 0.44 | 0.54 | 0.63 | 0.47 | 0.55 | 0.40 | ||
Gd | 2.38 | 1.89 | 2.38 | 1.51 | 1.61 | 1.67 | 2.42 | 1.16 | 2.43 | 1.93 | ||
Tb | 0.33 | 0.28 | 0.39 | 0.23 | 0.22 | 0.23 | 0.36 | 0.15 | 0.41 | 0.31 | ||
Dy | 1.68 | 1.42 | 2.15 | 1.34 | 1.18 | 1.16 | 1.93 | 0.73 | 2.39 | 1.75 | ||
Ho | 0.31 | 0.27 | 0.41 | 0.26 | 0.22 | 0.21 | 0.36 | 0.14 | 0.43 | 0.34 | ||
Er | 0.98 | 0.90 | 1.29 | 0.81 | 0.68 | 0.70 | 1.11 | 0.43 | 1.36 | 1.02 | ||
Tm | 0.18 | 0.17 | 0.23 | 0.15 | 0.13 | 0.13 | 0.20 | 0.08 | 0.25 | 0.18 | ||
Yb | 1.19 | 1.24 | 1.56 | 0.93 | 0.92 | 0.94 | 1.32 | 0.60 | 1.53 | 1.14 | ||
Lu | 0.19 | 0.22 | 0.25 | 0.15 | 0.14 | 0.17 | 0.21 | 0.11 | 0.25 | 0.17 | ||
Zr/Hf | 23.90 | 29.00 | 11.34 | 21.17 | 27.10 | 28.99 | 21.75 | 23.75 | 23.77 | 27.30 | ||
Nb/Ta | 11.60 | 13.28 | 74.63 | 13.75 | 14.84 | 12.39 | 12.54 | 15.89 | 13.80 | 11.31 | ||
Rb/Sr | 0.41 | 0.56 | 0.26 | 1.08 | 1.19 | 0.51 | 0.58 | 1.15 | 2.34 | 0.50 | ||
10000Ga/Al | 2.49 | 2.47 | 2.52 | 2.11 | 2.08 | 2.30 | 2.42 | 2.45 | 2.35 | 2.21 | ||
(La/Yb)N | 21.07 | 15.89 | 9.91 | 9.82 | 12.75 | 15.31 | 11.68 | 21.79 | 8.48 | 9.96 | ||
δEu | 0.66 | 0.78 | 0.51 | 0.48 | 0.80 | 0.89 | 0.70 | 1.18 | 0.62 | 0.55 | ||
Kfs | 48 | 50 | 52 | 52 | 70 | 35 | 45 | 40 | 40 | 42 | ||
Pl | 20 | 20 | 22 | 18 | 3 | 30 | 25 | 32 | 32 | 30 | ||
Q | 27 | 26 | 22 | 28 | 27 | 30 | 28 | 25 | 23 | 25 | ||
Bt | 5 | 4 | 2 | 2 | <1 | 5 | 2 | 3 | 5 | 3 |
图5 阿里河镇岩体SiO2-K2O ((a)底图据文献[31]) 和A/CNK-A/NK图解 ((b)底图据文献[33]) (大兴安岭花岗岩数据引自文献[11,13,23,34]; 东南沿海早白垩世高分异花岗岩数据引自文献[35?-37];图7—图9数据来源同)
Fig.5 SiO2-K2O ((a) basemap after ref.[31]) and A/CNK-A/NK ((b) basemap after ref.[33]) diagrams of the Alihe granites
图6 阿里河镇岩体微量元素原始地幔标准化蛛网图((a)原始地幔数据来自文献[38]) 和稀土元素球粒陨石标准化配分图((b)球粒陨石数据来自文献[39])
Fig.6 Primitive mantle-normalized trace element spidergram ((a), normalizing data from ref.[38]) and chondrite-normaized REE patterns ((b), normalizing data from ref.[39]) of the Alihe granites
图8 阿里河镇岩体的10000Ga/Al-FeOT/MgO图解(a)和(Zr+Nb+Ce+Y)-(K2O+Na2O)/CaO图解(b)(底图据文献[45]) FG.分异的长英质花岗岩;OGT.未分异的M、I、S花岗岩
Fig.8 10000Ga/Al-FeOT/MgO (a) and (Zr+Nb+Ce+Y)-(K2O+Na2O)/CaO (b) diagrams for the Alihe granites (basemap after ref.[45])
图9 阿里河镇岩体的Sr-Ba (a)和La-(La/Yb)N (b)关系图及分离结晶趋势 (a)图中Sr、Ba在斜长石中的分配系数据文献[47], 在其余矿物中的分配系数据文献[48], (b)图中副矿物分离结晶趋势线据文献[24]。PlAn10.斜长石(An=10);PlAn50.斜长石(An=50);Kfs.钾长石;Bt.黑云母;Amp.角闪石;Grt.石榴子石;Zr.锆石;Sph.榍石;Ap.磷灰石;Mon.独居石;Allan.褐帘石
Fig.9 Sr-Ba (a) and La-(La/Yb)N (b) diagrams showing the fractionation trends of the Alihe granites
图10 阿里河镇岩体的Rb/30-Hf-3Ta图解((a),底图据文献[70])和(Y+Nb)-Rb图解((b),底图据文献[71])
Fig.10 Ternary Rb/30-Hf-3Ta (a) and (Y+Nb)-Rb (b) diagrams for the Alihe granites (basemaps after refs.[70] and [71], respectively)
[1] | 吴福元, 孙德有, 林强. 东北地区显生宙花岗岩的成因与地壳增生[J]. 岩石学报, 1999, 15(2): 181-189. |
[2] | 曾涛, 王涛, 童英, 等. 俄罗斯远东地区晚中生代花岗岩类的时空分布及地质意义[J]. 地质通报, 2012, 31(5): 732-744. |
[3] | 周漪, 葛文春, 王清海. 大兴安岭中部乌兰浩特地区中生代花岗岩的成因: 地球化学及Sr-Nd-Hf同位素制约[J]. 岩石矿物学杂志, 2011, 30(5): 901-923. |
[4] | 孙德有, 吴福元, 李惠民, 等. 小兴安岭西北部造山后A型花岗岩的时代及与索伦山—贺根山—扎赉特碰撞拼合带东延的关系[J]. 科学通报, 2000, 45(20): 2217-2222. |
[5] | 孙德有, 吴福元, 林强, 等. 张广才岭燕山早期白石山岩体成因与壳幔相互作用[J]. 岩石学报, 2001, 17(2): 227-235. |
[6] | 孙德有, 吴福元, 高山, 等. 吉林中部晚三叠世和早侏罗世两期铝质A型花岗岩的厘定及对吉黑东部构造格局的制约[J]. 地学前缘, 2005, 12(2): 263-275. |
[7] | 葛文春, 吴福元, 周长勇, 等. 大兴安岭北部塔河花岗岩体的时代及对额尔古纳地块构造归属的制约[J]. 科学通报, 2005, 50 (12): 1239-1247. |
[8] | 葛文春, 吴福元, 周长勇, 等. 大兴安岭中部乌兰浩特地区中生代花岗岩的锆石U-Pb年龄及地质意义[J]. 岩石学报, 2005, 21(3): 749-762. |
[9] | 葛文春, 隋振民, 吴福元, 等. 大兴安岭东北部早古生代花岗岩锆石U-Pb年龄、Hf同位素特征及地质意义[J]. 岩石学报, 2007, 23(2): 423-440. |
[10] | 隋振民, 葛文春, 吴福元, 等. 大兴安岭东北部哈拉巴奇花岗岩体锆石U-Pb年龄及其成因[J]. 世界地质, 2006, 25(3): 229-236. |
[11] | 隋振民, 葛文春, 吴福元, 等. 大兴安岭东北部侏罗纪花岗质岩石的锆石U-Pb年龄、地球化学特征及成因[J]. 岩石学报, 2007, 23(2): 461-480. |
[12] | 佘宏全, 李进文, 向安平, 等. 大兴安岭中北段原岩锆石U-Pb测年及其与区域构造演化关系[J]. 岩石学报, 2012, 28(2): 571-594. |
[13] | 杨奇荻, 郭磊, 王涛, 等. 大兴安岭中南段甘珠尔庙地区晚中生代两期花岗岩的时代、成因、物源及其构造背景[J]. 岩石学报, 2014, 30(7): 1961-1981. |
[14] |
WU F Y, SUN D Y, GE W C, et al. Geochronology of the Phanerozoic granitoids in northeastern China[J]. Journal of Asian Earth Sciences, 2011, 41(1): 1-30.
DOI URL |
[15] |
WANG T, GUO L, ZHANG L, et al. Timing and evolution of Jurassic-Cretaceous granitoid magmatisms in the Mongol-Okhotsk belt and adjacent areas, NE Asia: Implications for transition from contractional crustal thickening to extensional thinning and geodynamic settings[J]. Journal of Asian Earth Sciences, 2015, 97: 365-392.
DOI URL |
[16] | 司秋亮, 崔天日, 唐振, 等. 大兴安岭中段柴河地区玛尼吐组火山岩年代学、地球化学及岩石成因[J]. 吉林大学学报(地球科学版), 2015, 45(2): 389-403. |
[17] | 宋立忠, 赵泽辉, 焦贵浩, 等. 松辽盆地早白垩世火山岩地球化学特征及其构造意义[J]. 岩石学报, 2010, 26(4): 1182-1194. |
[18] | 孙德有, 苟军, 任云生, 等. 满洲里南部玛尼吐组火山岩锆石U-Pb年龄与地球化学研究[J]. 岩石学报, 2011, 27(10): 3083-3094. |
[19] | 张吉衡. 大兴安岭中生代火山岩年代学及地球化学研究[D]. 武汉: 中国地质大学, 2009: 1-105. |
[20] |
TANG J, XU W L, WANG F, et al. Geochronology, geochemistry, and deformation history of Late Jurassic-Early Cretaceous intrusive rocks in the Erguna Massif, NE China: Constraints on the late Mesozoic tectonic evolution of the Mongol-Okhotsk orogenic belt[J]. Tectonophysics, 2015, 658: 91-110.
DOI URL |
[21] | 张旗, 潘国强, 李承东, 等. 花岗岩结晶分离作用问题: 关于花岗岩研究的思考之二[J]. 岩石学报, 2007, 23(6): 1239-1251. |
[22] |
WU F Y, LIU X C, JI W Q, et al. Highly fractionated granites: Recognition and research[J]. Science China Earth Sciences, 2017, 60(7): 1201-1219.
DOI URL |
[23] | 赵辉, 李舢, 王涛, 等. 大兴安岭南段黄岗梁地区早白垩世岩浆作用的时代、成因及其构造意义[J]. 地质通报, 2015, 34(12): 2203-2218. |
[24] |
WU F Y, JAHN B M, WILDE S A, et al. Highly fractionated I-type granites in NE China (I): geochronology and petrogenesis[J]. Lithos, 2003, 66(3/4): 241-273.
DOI URL |
[25] |
WU F Y, JAHN B M, Wilde S A, et al. Highly fractionated I-type granites in NE China (Ⅱ): isotopic geochemistry and implications for crustal growth in the Phanerozoic[J]. Lithos, 2003, 67(3/4): 191-204.
DOI URL |
[26] | 付俊彧, 刘英才, 赵春荆, 等. 东北地区大地构造相图(1∶150万)说明书[M]. 北京: 地质出版社, 2018: 21-63. |
[27] | 李怀坤, 耿建珍, 郝爽, 等. 用激光烧蚀多接收器等离子体质谱仪(LA-MC-ICPMS)测定锆石U-Pb同位素年龄的研究[J]. 矿物学报, 2009, 29(增): 600-601. |
[28] |
ANDERSEN T. Correction of common lead in U-Pb analyses that do not report 204Pb[J]. Chemical Geology, 2002, 192(1/2): 59-79.
DOI URL |
[29] |
LIU Y S, GAO S, HU Z C, et al. Continental and oceanic crust recycling-induced melt-peridotite interactions in the trans-north China orogen: U-Pb dating, Hf isotopes and trace elements in zircons from mantle xenoliths[J]. Journal of Petrology, 2010, 51(1/2): 537-571.
DOI URL |
[30] | LUDWIG K R. Isoplot/Ex Version 3.0: A Geochronological Toolkit for Microsoft Excel[M]. Berkeley: Berkeley Geochronology Center, 2003. |
[31] |
HOSKIN P W O, BLACK L P. Metamorphic zircon formation by solid-state recrystallization of protolith igneous zircon[J]. Journal of Metamorphic Geology, 2000, 18(4): 423-439.
DOI URL |
[32] |
PECCERILLO A, TAYLOR S R. Geochemistry of Eocene calc-alkaline volcanic rocks from the Kastamonu area, Northern Turkey[J]. Contributions to Mineralogy and Petrology, 1976, 58(1): 63-81.
DOI URL |
[33] |
MANIAR P D, PICCOLI P M. Tectonic discrimination of grani-toids[J]. Geological Society of America Bulletin, 1989, 101(5): 635-643.
DOI URL |
[34] | 徐立明, 王大可, 刘玉, 等. 大兴安岭北段塔河南部早白垩世侵入岩年代学和地球化学[J]. 现代地质, 2018, 32(6): 1212-1226. |
[35] | 李洁, 黄小龙. 江西雅山花岗岩岩浆演化及其Ta-Nb富集机制[J]. 岩石学报, 2013, 29(12): 4311-4322. |
[36] | 邱检生, 胡建, 王孝磊, 等. 广东河源白石冈岩体:一个高分异的I型花岗岩[J]. 地质学报, 2005, 79(4): 503-514. |
[37] | 邱检生, 肖娥, 胡建, 等. 福建北东沿海高分异I型花岗岩的成因:锆石U-Pb年代学、地球化学和Nd-Hf同位素制约[J]. 岩石学报, 2008, 24(11): 2468-2484. |
[38] |
SUN S S, MCDONOUGH W F. Chemical and isotopic systematics of oceanic basalts: Implications for mantle composition and processes[J]. Geological Society, London, Special Publications, 1989, 42(1): 313-345.
DOI URL |
[39] | BOYNTON W V. Cosmochemistry of the rare earth elements: Meteorite studies[M]//Rare Earth Element Geochemistry. Amsterdam: Elsevier, 1984: 63-114. |
[40] | 王玉往, 陈伟民, 李德东, 等. 内蒙古嘎仙钴镍硫化物矿床的地质特征及成因探讨[J]. 矿产勘查, 2016, 7(1): 72-81. |
[41] |
ZHU D C, MO X X, WANG L Q, et al. Petrogenesis of highly fractionated I-type granites in the Zayu area of eastern Gangdese, Tibet: Constraints from zircon U-Pb geochronology, geochemistry and Sr-Nd-Hf isotopes[J]. Science in China (Series D Earth Sciences), 2009, 52(9): 1223-1239.
DOI URL |
[42] | 陈璟元, 杨进辉. 佛冈高分异I型花岗岩的成因: 来自Nb-Ta-Zr-Hf等元素的制约[J]. 岩石学报, 2015, 31(3): 846-854. |
[43] |
LI X H, LI Z X, LI W X, et al. U-Pb zircon, geochemical and Sr-Nd-Hf isotopic constraints on age and origin of Jurassic I- and A-type granites from central Guangdong, SE China: A major igneous event in response to foundering of a subducted flat-slab?[J]. Lithos, 2007, 96(1/2): 186-204.
DOI URL |
[44] |
CHAPPELL B W. Aluminium saturation in I- and S-type granites and the characterization of fractionated haplogranites[J]. Lithos, 1999, 46(3): 535-551.
DOI URL |
[45] |
WHALEN J B, CURRIE K L, CHAPPELL B W. A-type granites: Geochemical characteristics, discrimination and petrogenesis[J]. Contributions to Mineralogy and Petrology, 1987, 95(4): 407-419.
DOI URL |
[46] |
CHAPPELL B W, WYBORN D. Cumulate and cumulative gra-nites and associated rocks[J]. Resource Geology, 2004, 54(3): 227-240.
DOI URL |
[47] |
BLUNDY J D, SHIMIZU N. Trace element evidence for plagioclase recycling in calc-alkaline magmas[J]. Earth and Planetary Science Letters, 1991, 102(2): 178-197.
DOI URL |
[48] |
EWART A, GRIFFIN W L. Application of proton-microprobe data to trace-element partitioning in volcanic rocks[J]. Chemical Geology, 1994, 117(1/2/3/4): 251-284.
DOI URL |
[49] |
KRAVCHINSKY V A, COGNÉ J P, HARBERT W P, et al. Evolution of the Mongol-Okhotsk Ocean as constrained by new palaeomagnetic data from the Mongol-Okhotsk suture zone, Siberia[J]. Geophysical Journal International, 2002, 148(1): 34-57.
DOI URL |
[50] | SOROKIN A A, KOTOV A B, KUDRYASHOV N M, et al. Late Paleozoic Urusha magmatic complex in the southern framing of the Mongolia-Okhotsk Belt (Amur Region): Age and geodynamic setting[J]. Petrology, 2005, 13: 596-610. |
[51] |
XIAO W J, WINDLEY B F, HUANG B C, et al. End-Permian to mid-Triassic termination of the accretionary processes of the southern Altaids: Implications for the geodynamic evolution, Phanerozoic continental growth, and metallogeny of Central Asia[J]. International Journal of Earth Sciences, 2009, 98(6): 1219-1220.
DOI URL |
[52] |
XU W L, PEI F P, WANG F, et al. Spatial-temporal relationships of Mesozoic volcanic rocks in NE China: Constraints on tectonic overprinting and transformations between multiple tectonic regimes[J]. Journal of Asian Earth Sciences, 2013, 74: 167-193.
DOI URL |
[53] |
ZORIN Y A. Geodynamics of the western part of the Mongolia-Okhotsk collisional belt, Trans-Baikal region (Russia) and Mongolia[J]. Tectonophysics, 1999, 306 (1): 33-56.
DOI URL |
[54] | 李锦轶, 莫申国, 和政军, 等. 大兴安岭北段地壳左行走滑运动的时代及其对中国东北及邻区中生代以来地壳构造演化重建的制约[J]. 地学前缘, 2004, 11(3): 157-168. |
[55] | 李锦轶, 曲军峰, 张进, 等. 中国北方造山区显生宙地质历史重建与成矿地质背景研究进展[J]. 地质通报, 2013, 32(增): 207-219. |
[56] |
SETON M, MÜLLER R D, ZAHIROVIC S, et al. Global continental and ocean basin reconstructions since 200 Ma[J]. Earth-Science Reviews, 2012, 113(3/4): 212-270.
DOI URL |
[57] |
TOMURTOGOO O, WINDLEY B F, KRONER A, et al. Zircon age and occurrence of the Adaatsag ophiolite and Muron shear zone, central Mongolia: Constraints on the evolution of the Mongol-Okhotsk Ocean, suture and orogen[J]. Journal of the Geological Society, 2005, 162(1): 125-134.
DOI URL |
[58] |
DONSKAYA T V, WINDLEY B F, MAZUKABZOV A M, et al. Age and evolution of Late Mesozoic metamorphic core complexes in southern Siberia and northern Mongolia[J]. Journal of the Geological Society, 2008, 165(1): 405-421.
DOI URL |
[59] |
COGNÉ J P, KRAVCHINSKY V A, HALIM N, et al. Late Jurassic-Early Cretaceous closure of the Mongol-Okhotsk Ocean demonstrated by new Mesozoic palaeomagnetic results from the Trans-Baïkal area (SE Siberia)[J]. Geophysical Journal International, 2005, 163(2): 813-832.
DOI URL |
[60] |
YANG Y T, GUO Z X, SONG C C, et al. A short-lived but significant Mongol-Okhotsk collisional orogeny in latest Jurassic-earliest Cretaceous[J]. Gondwana Research, 2015, 28(3): 1096-1116.
DOI URL |
[61] |
DONSKAYA T V, GLADKOCHUB D P, MAZUKABZOV A M, et al. Late Paleozoic-Mesozoic subduction-related magmatism at the southern margin of the Siberian continent and the 150 million-year history of the Mongol-Okhotsk Ocean[J]. Journal of Asian Earth Sciences, 2013, 62: 79-97.
DOI URL |
[62] | 张旗. 中国东部中生代岩浆活动与太平洋板块向西俯冲有关吗?[J]. 岩石矿物学杂志, 2013, 32(1): 113-128. |
[63] |
MENG Q R. What drove late Mesozoic extension of the Northern China-Mongolia tract?[J]. Tectonophysics, 2003, 369(3/4): 155-174.
DOI URL |
[64] |
GRAHAM S A, HENDRIX M S, JOHNSON C L, et al. Sedimentary record and tectonic implications of Mesozoic rifting in southeast Mongolia[J]. Geological Society of America Bulletin, 2001, 113(12): 1560-1579.
DOI URL |
[65] |
MENG Q R, HU J M, JIN J Q, et al. Tectonics of the late Mesozoic wide extensional basin system in the China-Mongolia border region[J]. Basin Research, 2003, 15(3): 397-415.
DOI URL |
[66] |
CHARLES N, AUGIER R, GUMIAUX C, et al. Timing, duration and role of magmatism in wide rift systems: Insights from the Jiaodong Peninsula (China, East Asia)[J]. Gondwana Research, 2013, 24(1): 412-428.
DOI URL |
[67] |
DAOUDENE Y, RUFFET G, COCHERIE A, et al. Timing of exhumation of the Ereendavaa metamorphic core complex (north-eastern Mongolia):U-Pb and 40Ar/39Ar constraints[J]. Journal of Asian Earth Sciences, 2013, 62: 98-116.
DOI URL |
[68] |
WU F Y, SUN D Y, LI H M, et al. A-type granites in north-eastern China: Age and geochemical constraints on their petroge-nesis[J]. Chemical Geology, 2002, 187(1/2): 143-173.
DOI URL |
[69] |
WU F Y, LIN J Q, WILDE S A, et al. Nature and significance of the Early Cretaceous giant igneous event in Eastern China[J]. Earth and Planetary Science Letters, 2005, 233(1/2): 103-119.
DOI URL |
[70] | HARRIS N B W, PEARCE J A, TINDLE A G. Geochemical characteristics of collision-zone magmatism[J]. Geological So-ciety, London, Special Publications, 1986, 19(1): 67-81. |
[71] |
PEARCE J. Sources and settings of granitic rocks[J]. Episodes, 1996, 19(4): 120-125.
DOI URL |
[1] | 李柱, 张德会, 张荣臻, 沈存利, 焦世豪, 李林, 朱鹏龙. 内蒙古那仁乌拉早白垩世高分异花岗岩年代学及其成因[J]. 现代地质, 2022, 36(03): 848-861. |
[2] | 周桐, 孙珍军, 于赫楠, 王承洋, 刘广虎. 内蒙古浩布高铅锌矿床小罕山岩体年代学、Hf同位素及地球化学特征[J]. 现代地质, 2022, 36(01): 282-294. |
[3] | 刘爱荣, 徐永婧, 刘成林, 庞尔成. 大同盆地地质特征及构造演化研究[J]. 现代地质, 2021, 35(05): 1296-1310. |
[4] | 刘畅, 杨竹森, 徐培言, 赵晓燕, 夏文杰, 杨晓旭. 冈底斯西段麻木矽卡岩型铅锌矿化区岩浆岩锆石U-Pb年龄及地质意义[J]. 现代地质, 2021, 35(02): 466-476. |
[5] | 侯江龙, 李建康, 王登红, 代鸿章, 刘丽君. 四川甲基卡锂矿区二长花岗岩的地球化学、氢氧同位素组成及其地质意义[J]. 现代地质, 2020, 34(05): 1058-1066. |
[6] | 杨元江, 李成禄, 邓昌州, 李文龙, 张立, 赵忠海, 赵寒冬. 大兴安岭大洋山钼矿成矿岩体地球化学、锆石U-Pb年龄及构造背景[J]. 现代地质, 2020, 34(05): 1092-1102. |
[7] | 宓奎峰, 杨艳, 颜廷杰, 吕志成, 柳振江. 内蒙古沙麦钨矿区高分异花岗岩独居石U-Pb定年及成矿意义[J]. 现代地质, 2020, 34(03): 504-513. |
[8] | 王伟, 王生云, 刘涛, 李天石, 陈云杰, 马骊, 赵如意, 宋振涛. 甘肃红石泉伟晶岩型铀矿床地质、地球化学特征及成因探讨[J]. 现代地质, 2020, 34(02): 244-253. |
[9] | 滕超, 张晓飞, 周毅, 冯俊岭, 李树才. 内蒙古锡林浩特小乌兰沟早白垩世二长花岗岩LA-ICP-MS锆石U-Pb年龄及其地质意义[J]. 现代地质, 2019, 33(05): 1003-1014. |
[10] | 魏永峰, 肖倩茹, 李有波, 罗巍, 冉杰, 林美英. 西藏纳木错早白垩世流纹岩锆石U-Pb年龄、地球化学及其构造意义[J]. 现代地质, 2019, 33(03): 487-500. |
[11] | 徐立明, 王大可, 刘玉, 郑吉林, 张文强, 梁中恺. 大兴安岭北段塔河南部早白垩世侵入岩年代学和地球化学[J]. 现代地质, 2018, 32(06): 1212-1226. |
[12] | 刘刚, 刘家军, 袁峰, 张帅, 沙亚洲, 张宏远, 王功文. 陕西小花岔铀矿床岩浆演化及其对铀成矿作用的制约[J]. 现代地质, 2017, 31(05): 990-1005. |
[13] | 冉怀江,范乐元,胡圣利,尤征,金博. 苏丹Muglad盆地凯康凹陷西斜坡早白垩世沉积层序及其控制因素研究[J]. 现代地质, 2014, 28(4): 799-805. |
[14] | 张英志,林畅松,高志勇,芦刚,任宇泽,宋宁宁,霍志达. 塔西南坳陷早白垩世物源体系和沉积古地理分析[J]. 现代地质, 2014, 28(4): 791-798. |
[15] | 胡鸿飞,戴霜. 六盘山地区早白垩世磁性地层年代及其构造意义[J]. 现代地质, 2013, 27(2): 278-287. |
阅读次数 | ||||||
全文 |
|
|||||
摘要 |
|
|||||