现代地质 ›› 2022, Vol. 36 ›› Issue (01): 244-258.DOI: 10.19657/j.geoscience.1000-8527.2020.047
刘建栋1,2(), 李五福1,2(
), 王国良1,2, 董进生1,2, 曹锦山1,2, 李红刚1,2, 赵忠国1,2
收稿日期:
2018-12-19
修回日期:
2020-04-16
出版日期:
2022-02-10
发布日期:
2022-03-08
通讯作者:
李五福
作者简介:
李五福,男,硕士,高级工程师,1982年出生,构造地质学专业,从事区域地质调查研究工作。Email: 15422504@qq.com。基金资助:
LIU Jiandong1,2(), LI Wufu1,2(
), WANG Guoliang1,2, DONG Jinshen1,2, CAO Jinshan1,2, LI Honggang1,2, ZHAO Zhongguo1,2
Received:
2018-12-19
Revised:
2020-04-16
Online:
2022-02-10
Published:
2022-03-08
Contact:
LI Wufu
摘要:
为加强对北祁连早古生代多岛弧盆系蛇绿混杂岩的调查,选取柏木峡—门岗峡蛇绿岩开展岩相学、年代学和地球化学研究。柏木峡—门岗峡蛇绿岩位于青海省海东市互助县,构造上处于北祁连造山带中东段。由橄榄岩、辉长岩和基性火山岩组成较为完整的蛇绿岩单元。对辉长岩进行单颗粒锆石LA-ICP-MS U-Pb同位素测年,获得206Pb/238U加权平均年龄为(525.2±1.1) Ma(MSWD=0.06),代表了蛇绿岩的形成年龄,相当于早寒武世。岩石地球化学研究表明,该蛇绿岩中的基性火山岩属于拉斑系列,具有洋岛玄武岩的地球化学特征;玄武岩Th/Yb-Nb/Yb和TiO2/Yb-Nb/Yb等构造环境判别图显示,该套蛇绿岩的形成环境与俯冲作用无关。结合详细的野外调查和区域对比,认为该蛇绿岩代表早古生代北祁连洋壳,与玉石沟—川刺沟等蛇绿岩共同构成了达坂山—玉石沟蛇绿岩带。
中图分类号:
刘建栋, 李五福, 王国良, 董进生, 曹锦山, 李红刚, 赵忠国. 北祁连东段柏木峡—门岗峡地区蛇绿岩的识别及其区域构造意义[J]. 现代地质, 2022, 36(01): 244-258.
LIU Jiandong, LI Wufu, WANG Guoliang, DONG Jinshen, CAO Jinshan, LI Honggang, ZHAO Zhongguo. Identification of Ophiolites in the Baimuxia-Mengangxia Area in the Eastern Part of the North Qilian Mountains and Their Regional Tectonic Significance[J]. Geoscience, 2022, 36(01): 244-258.
图1 柏木峡—门岗峡地区地质简图④ (a)大地构造简图(兼示主要蛇绿岩位置及年龄);(b)研究区地质简图 ④青海省地质调查院.青海1∶5万玉龙滩等四幅区调区域地质调查报告.西宁:青海省地质调查院,2012.
Fig.1 Geological sketch of Baimuxia-Mengangxia area④
图3 柏木峡—门岗峡蛇绿混杂岩实测地质剖面图(剖面位置见图1) 1.英安质晶屑凝灰岩;2.凝灰岩;3.英安质凝灰岩;4.变晶屑玻屑凝灰岩;5.晶屑岩屑凝灰岩;6.沉凝灰岩;7.岩屑晶屑凝灰岩;8.晶屑凝灰岩;9.安山岩;10.英安质晶屑凝灰岩;11.含火山角砾岩屑凝灰岩;12.晶屑凝灰岩(夹灰绿色硅质岩);13.英安质晶屑凝灰岩;14.蚀变辉长岩;15.角闪阳起片岩;16.灰绿色辉长岩;17.深灰色蚀变辉长岩;18.深灰绿色蚀变玄武岩;19.深灰绿色变质玄武岩;20.灰黑色碎裂岩化蚀变辉长岩;21.深灰绿色碎裂化辉长岩;22.辉长岩;23.深灰绿色玄武岩;24.辉石岩;25.斜长角闪岩;26.角闪斜长岩;27.蛇纹石化橄榄辉长岩;28.灰绿色玄武岩;29.深灰色斜长角闪岩;30.黑色玄武岩;31.角闪斜长岩
Fig.3 Surveyed geological profile of ophiolite melange in Baimuxia-Mengangxia area (profile location seeing Fig.1)
图4 柏木峡—门岗峡蛇绿岩镜下显微照片 (a)(b)辉长岩镜下显微特征;(c)(d)玄武岩镜下显微特征;Prx.辉石;Hb.角闪石;Pl.斜长石;Ep.绿帘石;Qz.石英;Act.阳起石;Bi.黑云母;Mt.磁铁矿
Fig.4 Microscopic photos of ophiolite outcrop in Baimuxia-Mengangxin area
序号 | Pb /10-6 | U /10-6 | 同位素比值 | 年龄/Ma | |||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
206Pb/ 238U | 207Pb/ 235U | 207Pb/ 206Pb | 208Pb/ 232Th | 232Th/ 238U | 206Pb/ 238U | 1σ | 207Pb/ 235U | 1σ | 207Pb/ 206Pb | 1σ | |||
1 | 9 | 106 | 0.084 6 | 0.676 2 | 0.058 0 | 0.039 9 | 0.215 0 | 523 | 3 | 524 | 15 | 529 | 61 |
2 | 11 | 131 | 0.084 9 | 0.676 7 | 0.057 8 | 0.030 8 | 0.366 0 | 525 | 3 | 525 | 11 | 522 | 48 |
3 | 21 | 235 | 0.084 9 | 0.677 9 | 0.057 9 | 0.029 4 | 0.469 7 | 525 | 3 | 525 | 7 | 527 | 30 |
4 | 11 | 126 | 0.084 9 | 0.677 3 | 0.057 9 | 0.030 7 | 0.310 4 | 525 | 3 | 525 | 10 | 525 | 40 |
5 | 33 | 351 | 0.084 9 | 0.677 9 | 0.057 9 | 0.029 2 | 0.667 7 | 525 | 3 | 526 | 5 | 528 | 22 |
6 | 24 | 262 | 0.085 0 | 0.678 0 | 0.057 9 | 0.028 6 | 0.527 5 | 526 | 3 | 526 | 6 | 525 | 26 |
7 | 34 | 358 | 0.085 0 | 0.679 3 | 0.058 0 | 0.030 5 | 0.601 0 | 526 | 3 | 526 | 6 | 529 | 26 |
8 | 35 | 378 | 0.084 8 | 0.673 5 | 0.057 6 | 0.031 9 | 0.565 3 | 525 | 3 | 523 | 6 | 516 | 24 |
9 | 8 | 93 | 0.084 7 | 0.677 8 | 0.058 0 | 0.033 2 | 0.319 9 | 524 | 3 | 525 | 18 | 531 | 76 |
10 | 19 | 215 | 0.084 7 | 0.677 2 | 0.058 0 | 0.031 3 | 0.466 1 | 524 | 3 | 525 | 8 | 528 | 34 |
11 | 15 | 165 | 0.085 0 | 0.679 4 | 0.058 0 | 0.031 4 | 0.396 7 | 526 | 3 | 526 | 11 | 529 | 45 |
12 | 31 | 320 | 0.084 7 | 0.677 3 | 0.058 0 | 0.034 4 | 0.644 8 | 524 | 3 | 525 | 6 | 530 | 24 |
13 | 22 | 242 | 0.084 9 | 0.679 4 | 0.058 1 | 0.030 6 | 0.543 8 | 525 | 3 | 526 | 7 | 532 | 31 |
14 | 8 | 97 | 0.084 8 | 0.677 9 | 0.058 0 | 0.031 5 | 0.354 0 | 525 | 3 | 526 | 14 | 529 | 57 |
15 | 5 | 58 | 0.084 8 | 0.679 0 | 0.058 1 | 0.038 1 | 0.148 5 | 525 | 5 | 526 | 23 | 532 | 86 |
16 | 17 | 193 | 0.084 7 | 0.677 1 | 0.058 0 | 0.030 1 | 0.448 5 | 524 | 3 | 525 | 9 | 529 | 39 |
17 | 7 | 82 | 0.085 1 | 0.679 0 | 0.057 9 | 0.032 0 | 0.324 0 | 526 | 3 | 526 | 16 | 525 | 67 |
18 | 8 | 90 | 0.084 9 | 0.676 9 | 0.057 9 | 0.027 7 | 0.334 8 | 525 | 3 | 525 | 14 | 524 | 58 |
19 | 14 | 180 | 0.084 8 | 0.675 4 | 0.057 8 | 0.029 3 | 0.062 8 | 525 | 3 | 524 | 8 | 521 | 31 |
20 | 14 | 157 | 0.084 9 | 0.680 3 | 0.058 1 | 0.028 9 | 0.481 7 | 525 | 3 | 527 | 9 | 534 | 38 |
21 | 21 | 228 | 0.085 0 | 0.677 5 | 0.057 8 | 0.032 6 | 0.468 7 | 526 | 3 | 525 | 8 | 521 | 34 |
22 | 10 | 109 | 0.085 0 | 0.678 6 | 0.057 9 | 0.032 7 | 0.347 8 | 526 | 3 | 526 | 14 | 525 | 55 |
23 | 8 | 92 | 0.084 9 | 0.679 0 | 0.058 0 | 0.031 3 | 0.271 6 | 525 | 3 | 526 | 15 | 531 | 61 |
24 | 36 | 349 | 0.084 8 | 0.678 2 | 0.058 0 | 0.021 9 | 1.294 2 | 525 | 3 | 526 | 19 | 529 | 78 |
25 | 11 | 121 | 0.085 0 | 0.676 6 | 0.057 7 | 0.038 9 | 0.293 2 | 526 | 3 | 525 | 13 | 519 | 54 |
26 | 18 | 192 | 0.085 0 | 0.679 0 | 0.057 9 | 0.033 5 | 0.627 6 | 526 | 4 | 526 | 10 | 528 | 39 |
27 | 1 | 16 | 0.085 3 | 0.850 2 | 0.072 3 | 0.028 4 | 0.106 0 | 528 | 6 | 625 | 85 | 995 | 293 |
28 | 8 | 93 | 0.084 9 | 0.678 9 | 0.058 0 | 0.031 6 | 0.250 1 | 525 | 3 | 526 | 18 | 529 | 73 |
29 | 11 | 121 | 0.085 2 | 0.679 7 | 0.057 9 | 0.034 0 | 0.412 1 | 527 | 4 | 527 | 22 | 524 | 90 |
30 | 10 | 113 | 0.085 0 | 0.679 9 | 0.058 0 | 0.031 2 | 0.346 5 | 526 | 3 | 527 | 17 | 531 | 69 |
31 | 10 | 117 | 0.084 8 | 0.678 7 | 0.058 0 | 0.026 9 | 0.369 2 | 525 | 3 | 526 | 12 | 531 | 51 |
32 | 8 | 98 | 0.084 8 | 0.676 1 | 0.057 8 | 0.029 5 | 0.342 3 | 525 | 3 | 524 | 15 | 523 | 62 |
表1 柏木峡—门岗峡辉长岩(IPm20JD(U-Pb)22-1)LA-ICP-MS锆石U-Pb年龄分析结果
Table 1 LA-ICP-MS zircons U-Pb dating data of gabbro(IPm20JD(U-Pb)22-1) from Baimuxia-Mengangxia ophiolite
序号 | Pb /10-6 | U /10-6 | 同位素比值 | 年龄/Ma | |||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
206Pb/ 238U | 207Pb/ 235U | 207Pb/ 206Pb | 208Pb/ 232Th | 232Th/ 238U | 206Pb/ 238U | 1σ | 207Pb/ 235U | 1σ | 207Pb/ 206Pb | 1σ | |||
1 | 9 | 106 | 0.084 6 | 0.676 2 | 0.058 0 | 0.039 9 | 0.215 0 | 523 | 3 | 524 | 15 | 529 | 61 |
2 | 11 | 131 | 0.084 9 | 0.676 7 | 0.057 8 | 0.030 8 | 0.366 0 | 525 | 3 | 525 | 11 | 522 | 48 |
3 | 21 | 235 | 0.084 9 | 0.677 9 | 0.057 9 | 0.029 4 | 0.469 7 | 525 | 3 | 525 | 7 | 527 | 30 |
4 | 11 | 126 | 0.084 9 | 0.677 3 | 0.057 9 | 0.030 7 | 0.310 4 | 525 | 3 | 525 | 10 | 525 | 40 |
5 | 33 | 351 | 0.084 9 | 0.677 9 | 0.057 9 | 0.029 2 | 0.667 7 | 525 | 3 | 526 | 5 | 528 | 22 |
6 | 24 | 262 | 0.085 0 | 0.678 0 | 0.057 9 | 0.028 6 | 0.527 5 | 526 | 3 | 526 | 6 | 525 | 26 |
7 | 34 | 358 | 0.085 0 | 0.679 3 | 0.058 0 | 0.030 5 | 0.601 0 | 526 | 3 | 526 | 6 | 529 | 26 |
8 | 35 | 378 | 0.084 8 | 0.673 5 | 0.057 6 | 0.031 9 | 0.565 3 | 525 | 3 | 523 | 6 | 516 | 24 |
9 | 8 | 93 | 0.084 7 | 0.677 8 | 0.058 0 | 0.033 2 | 0.319 9 | 524 | 3 | 525 | 18 | 531 | 76 |
10 | 19 | 215 | 0.084 7 | 0.677 2 | 0.058 0 | 0.031 3 | 0.466 1 | 524 | 3 | 525 | 8 | 528 | 34 |
11 | 15 | 165 | 0.085 0 | 0.679 4 | 0.058 0 | 0.031 4 | 0.396 7 | 526 | 3 | 526 | 11 | 529 | 45 |
12 | 31 | 320 | 0.084 7 | 0.677 3 | 0.058 0 | 0.034 4 | 0.644 8 | 524 | 3 | 525 | 6 | 530 | 24 |
13 | 22 | 242 | 0.084 9 | 0.679 4 | 0.058 1 | 0.030 6 | 0.543 8 | 525 | 3 | 526 | 7 | 532 | 31 |
14 | 8 | 97 | 0.084 8 | 0.677 9 | 0.058 0 | 0.031 5 | 0.354 0 | 525 | 3 | 526 | 14 | 529 | 57 |
15 | 5 | 58 | 0.084 8 | 0.679 0 | 0.058 1 | 0.038 1 | 0.148 5 | 525 | 5 | 526 | 23 | 532 | 86 |
16 | 17 | 193 | 0.084 7 | 0.677 1 | 0.058 0 | 0.030 1 | 0.448 5 | 524 | 3 | 525 | 9 | 529 | 39 |
17 | 7 | 82 | 0.085 1 | 0.679 0 | 0.057 9 | 0.032 0 | 0.324 0 | 526 | 3 | 526 | 16 | 525 | 67 |
18 | 8 | 90 | 0.084 9 | 0.676 9 | 0.057 9 | 0.027 7 | 0.334 8 | 525 | 3 | 525 | 14 | 524 | 58 |
19 | 14 | 180 | 0.084 8 | 0.675 4 | 0.057 8 | 0.029 3 | 0.062 8 | 525 | 3 | 524 | 8 | 521 | 31 |
20 | 14 | 157 | 0.084 9 | 0.680 3 | 0.058 1 | 0.028 9 | 0.481 7 | 525 | 3 | 527 | 9 | 534 | 38 |
21 | 21 | 228 | 0.085 0 | 0.677 5 | 0.057 8 | 0.032 6 | 0.468 7 | 526 | 3 | 525 | 8 | 521 | 34 |
22 | 10 | 109 | 0.085 0 | 0.678 6 | 0.057 9 | 0.032 7 | 0.347 8 | 526 | 3 | 526 | 14 | 525 | 55 |
23 | 8 | 92 | 0.084 9 | 0.679 0 | 0.058 0 | 0.031 3 | 0.271 6 | 525 | 3 | 526 | 15 | 531 | 61 |
24 | 36 | 349 | 0.084 8 | 0.678 2 | 0.058 0 | 0.021 9 | 1.294 2 | 525 | 3 | 526 | 19 | 529 | 78 |
25 | 11 | 121 | 0.085 0 | 0.676 6 | 0.057 7 | 0.038 9 | 0.293 2 | 526 | 3 | 525 | 13 | 519 | 54 |
26 | 18 | 192 | 0.085 0 | 0.679 0 | 0.057 9 | 0.033 5 | 0.627 6 | 526 | 4 | 526 | 10 | 528 | 39 |
27 | 1 | 16 | 0.085 3 | 0.850 2 | 0.072 3 | 0.028 4 | 0.106 0 | 528 | 6 | 625 | 85 | 995 | 293 |
28 | 8 | 93 | 0.084 9 | 0.678 9 | 0.058 0 | 0.031 6 | 0.250 1 | 525 | 3 | 526 | 18 | 529 | 73 |
29 | 11 | 121 | 0.085 2 | 0.679 7 | 0.057 9 | 0.034 0 | 0.412 1 | 527 | 4 | 527 | 22 | 524 | 90 |
30 | 10 | 113 | 0.085 0 | 0.679 9 | 0.058 0 | 0.031 2 | 0.346 5 | 526 | 3 | 527 | 17 | 531 | 69 |
31 | 10 | 117 | 0.084 8 | 0.678 7 | 0.058 0 | 0.026 9 | 0.369 2 | 525 | 3 | 526 | 12 | 531 | 51 |
32 | 8 | 98 | 0.084 8 | 0.676 1 | 0.057 8 | 0.029 5 | 0.342 3 | 525 | 3 | 524 | 15 | 523 | 62 |
图6 柏木峡—门岗峡辉长岩(IPm20JD(U-Pb)22-1)LA-ICP-MS锆石U-Pb谐和图
Fig.6 LA-ICP-MS zircons U-Pb concordia diagrams of gabbro(IPm20JD(U-Pb)22-1) from Baimuxia-Mengangxia ophiolite
岩性 | 样品号 | SiO2 | TiO2 | Al2O3 | Fe2O3 | FeO | MnO | MgO | CaO | Na2O | K2O | P2O5 | 烧失量 | 总量 |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
橄榄岩 | MGX01 | 35.07 | 0.07 | 1.17 | 5.46 | 3.27 | 0.12 | 28.90 | 8.68 | 0.02 | 0.03 | 0.02 | 16.08 | 98.89 |
MGX02 | 40.61 | 0.10 | 1.06 | 5.63 | 3.45 | 0.13 | 34.35 | 2.27 | 0.01 | 0.03 | 0.05 | 12.09 | 99.78 | |
MGX03 | 38.85 | 0.06 | 2.40 | 7.53 | 1.30 | 0.12 | 36.92 | 0.23 | 0.32 | 0.03 | 0.04 | 11.91 | 99.73 | |
辉长岩 | MGX04 | 46.16 | 0.34 | 15.51 | 1.35 | 5.08 | 0.10 | 11.18 | 14.27 | 0.81 | 0.10 | 0.05 | 4.88 | 99.83 |
MGX05 | 49.76 | 0.31 | 15.12 | 1.12 | 6.40 | 0.14 | 10.55 | 10.25 | 2.09 | 0.99 | 0.07 | 2.83 | 99.63 | |
MGX06 | 48.71 | 0.57 | 17.42 | 0.70 | 5.70 | 0.11 | 9.06 | 11.30 | 2.15 | 0.83 | 0.07 | 3.22 | 99.84 | |
MGX07 | 49.42 | 0.69 | 13.85 | 2.12 | 8.10 | 0.18 | 8.91 | 11.20 | 2.16 | 0.77 | 0.04 | 2.05 | 99.49 | |
MGX08 | 48.68 | 1.58 | 13.76 | 2.21 | 8.70 | 0.18 | 5.56 | 9.11 | 4.28 | 0.34 | 0.23 | 5.07 | 99.70 | |
MGX09 | 48.09 | 1.72 | 15.47 | 4.38 | 7.40 | 0.24 | 5.38 | 8.87 | 3.31 | 0.82 | 0.26 | 3.70 | 99.64 | |
MGX10 | 46.88 | 2.69 | 13.28 | 3.32 | 10.25 | 0.21 | 6.26 | 11.13 | 2.26 | 0.33 | 0.15 | 2.90 | 99.66 | |
MGX11 | 46.67 | 2.58 | 13.61 | 3.85 | 10.20 | 0.22 | 6.37 | 10.44 | 2.62 | 0.35 | 0.29 | 2.43 | 99.63 | |
MGX12 | 45.37 | 2.14 | 13.75 | 4.39 | 8.05 | 0.18 | 5.68 | 12.72 | 1.96 | 0.21 | 0.25 | 4.76 | 99.46 | |
MGX13 | 49.52 | 2.23 | 13.02 | 3.77 | 8.80 | 0.19 | 5.25 | 9.92 | 3.42 | 0.50 | 0.31 | 2.70 | 99.63 | |
MGX14 | 48.25 | 2.33 | 13.81 | 3.85 | 9.05 | 0.20 | 5.93 | 9.62 | 3.35 | 0.92 | 0.31 | 2.06 | 99.68 | |
玄武岩 | MGX15 | 49.74 | 2.14 | 13.25 | 3.25 | 8.90 | 0.17 | 5.07 | 9.67 | 3.41 | 0.47 | 0.28 | 2.93 | 99.28 |
MGX16 | 46.92 | 3.36 | 15.79 | 3.05 | 10.25 | 0.11 | 6.01 | 8.04 | 2.73 | 1.22 | 0.42 | 1.77 | 99.67 | |
MGX17 | 50.21 | 3.56 | 15.12 | 2.79 | 10.65 | 0.15 | 4.31 | 7.71 | 2.24 | 0.56 | 0.47 | 2.13 | 99.90 | |
MGX18 | 50.10 | 2.64 | 16.55 | 2.07 | 9.15 | 0.12 | 4.85 | 5.92 | 2.83 | 0.43 | 0.28 | 4.74 | 99.68 | |
MGX19 | 48.18 | 2.45 | 14.97 | 6.17 | 4.83 | 0.12 | 6.66 | 8.32 | 1.86 | 0.74 | 0.32 | 5.14 | 99.76 | |
MGX20 | 47.30 | 3.47 | 14.94 | 8.45 | 4.35 | 0.20 | 7.57 | 8.12 | 2.09 | 0.39 | 0.58 | 2.42 | 99.88 | |
MGX21 | 45.75 | 2.70 | 14.86 | 5.94 | 7.40 | 0.22 | 8.67 | 7.23 | 0.28 | 0.88 | 0.38 | 5.45 | 99.76 | |
岩性 | 样品号 | La | Ce | Pr | Nd | Sm | Eu | Gd | Tb | Dy | Ho | Er | Tm | Yb |
橄榄岩 | MGX01 | 2.00 | 3.22 | 0.44 | 1.71 | 0.28 | 0.17 | 0.28 | 0.05 | 0.25 | 0.05 | 0.13 | 0.02 | 0.14 |
MGX02 | 2.17 | 5.87 | 0.82 | 3.76 | 0.82 | 0.25 | 0.64 | 0.07 | 0.41 | 0.07 | 0.18 | 0.02 | 0.15 | |
MGX03 | 2.04 | 3.79 | 0.57 | 2.21 | 0.44 | 0.11 | 0.50 | 0.09 | 0.61 | 0.13 | 0.37 | 0.06 | 0.46 | |
辉长岩 | MGX04 | 2.91 | 6.73 | 0.80 | 4.58 | 1.22 | 0.47 | 1.21 | 0.18 | 1.13 | 0.23 | 0.60 | 0.08 | 0.53 |
MGX05 | 5.91 | 11.88 | 1.48 | 6.06 | 1.33 | 0.51 | 1.60 | 0.31 | 2.01 | 0.43 | 1.22 | 0.21 | 1.38 | |
MGX06 | 1.96 | 5.12 | 0.83 | 4.07 | 1.37 | 0.61 | 1.76 | 0.31 | 2.18 | 0.41 | 1.16 | 0.18 | 1.14 | |
MGX07 | 3.79 | 6.51 | 0.84 | 3.76 | 1.17 | 0.60 | 1.61 | 0.33 | 2.14 | 0.46 | 1.32 | 0.22 | 1.45 | |
MGX08 | 11.91 | 26.24 | 4.17 | 19.61 | 4.76 | 1.48 | 5.57 | 1.04 | 6.51 | 1.34 | 3.85 | 0.63 | 4.10 | |
MGX09 | 11.18 | 25.03 | 3.63 | 17.47 | 4.69 | 1.51 | 5.31 | 0.97 | 6.13 | 1.24 | 3.61 | 0.59 | 3.57 | |
MGX10 | 8.02 | 18.98 | 2.93 | 14.04 | 4.09 | 1.34 | 4.40 | 0.81 | 5.15 | 1.06 | 2.98 | 0.47 | 2.88 | |
MGX11 | 11.47 | 29.09 | 4.64 | 22.80 | 6.49 | 2.07 | 7.01 | 1.32 | 7.99 | 1.59 | 4.60 | 0.71 | 4.38 | |
MGX12 | 10.01 | 25.00 | 3.81 | 18.16 | 4.81 | 1.63 | 5.05 | 0.90 | 5.35 | 1.03 | 2.84 | 0.42 | 2.66 | |
MGX13 | 17.17 | 37.04 | 5.57 | 25.68 | 6.18 | 2.14 | 6.71 | 1.21 | 6.99 | 1.40 | 3.78 | 0.61 | 3.86 | |
MGX14 | 17.44 | 38.94 | 5.58 | 25.28 | 5.81 | 2.19 | 6.47 | 1.11 | 6.47 | 1.26 | 3.30 | 0.55 | 3.38 | |
玄武岩 | MGX15 | 13.67 | 30.34 | 4.67 | 22.00 | 5.37 | 1.87 | 6.26 | 1.13 | 6.74 | 1.35 | 3.63 | 0.59 | 3.81 |
MGX16 | 32.20 | 63.91 | 8.43 | 36.29 | 8.02 | 2.58 | 7.26 | 1.15 | 6.23 | 1.08 | 2.82 | 0.39 | 2.35 | |
MGX17 | 28.22 | 57.93 | 7.81 | 34.83 | 8.23 | 2.63 | 7.63 | 1.30 | 6.99 | 1.23 | 3.11 | 0.44 | 2.48 | |
MGX18 | 19.86 | 40.81 | 5.48 | 24.71 | 6.17 | 2.11 | 6.21 | 1.04 | 5.59 | 1.00 | 2.4 | 0.35 | 1.93 | |
MGX19 | 22.77 | 43.96 | 5.63 | 24.46 | 5.82 | 1.79 | 5.53 | 0.89 | 4.93 | 0.88 | 2.29 | 0.32 | 1.75 | |
MGX20 | 34.71 | 72.39 | 9.50 | 41.05 | 9.00 | 2.95 | 7.43 | 1.11 | 5.42 | 0.91 | 2.10 | 0.28 | 1.56 | |
MGX21 | 22.79 | 49.71 | 6.60 | 28.82 | 6.53 | 2.18 | 6.62 | 0.99 | 5.39 | 0.98 | 2.45 | 0.33 | 2.00 | |
岩性 | 样品号 | Lu | Y | Sr | Rb | Ba | Th | Ta | Nb | Zr | Hf | Ti | K | P |
橄榄岩 | MGX01 | 0.02 | 1.39 | 63.50 | 1.83 | 206.70 | 0.44 | 0.07 | 0.46 | 6.80 | 0.18 | 507 | 301 | 105 |
MGX02 | 0.02 | 2.05 | 12.84 | 0.63 | 68.77 | 0.31 | 0.26 | 0.66 | 12.79 | 0.47 | 684 | 284 | 249 | |
MGX03 | 0.07 | 3.36 | 12.60 | 2.97 | 8.90 | 1.10 | 0.10 | 0.80 | 9.60 | 0.32 | 410 | 284 | 199 | |
辉长岩 | MGX04 | 0.07 | 5.66 | 395.50 | 1.55 | 47.94 | 0.37 | 0.33 | 0.85 | 15.06 | 0.63 | 2 147 | 874 | 230 |
MGX05 | 0.21 | 10.74 | 298.70 | 37.78 | 191.70 | 2.36 | 0.24 | 2.02 | 24.00 | 0.80 | 1 920 | 8 490 | 316 | |
MGX06 | 0.15 | 11.31 | 275.50 | 30.32 | 122.60 | 1.29 | 0.39 | 2.05 | 32.78 | 1.27 | 3 537 | 7 131 | 316 | |
MGX07 | 0.21 | 11.21 | 182.00 | 2.39 | 194.10 | 0.85 | 0.29 | 1.28 | 19.40 | 0.65 | 4 245 | 6 560 | 179 | |
MGX08 | 0.60 | 33.59 | 204.50 | 5.84 | 82.80 | 1.04 | 0.73 | 8.95 | 156.20 | 5.21 | 10 010 | 2 983 | 1 061 | |
MGX09 | 0.54 | 33.12 | 427.40 | 10.69 | 355.50 | 0.17 | 0.93 | 12.74 | 128.50 | 3.71 | 10 748 | 7 095 | 1 183 | |
MGX10 | 0.41 | 28.61 | 225.70 | 5.95 | 136.10 | 0.61 | 0.60 | 7.85 | 107.00 | 2.96 | 16 667 | 2 831 | 677 | |
MGX11 | 0.63 | 42.66 | 251.40 | 2.95 | 166.40 | 0.38 | 0.93 | 11.80 | 167.00 | 5.75 | 15 913 | 2 989 | 1 302 | |
MGX12 | 0.37 | 27.38 | 465.70 | 1.34 | 152.70 | 0.13 | 0.94 | 13.62 | 126.60 | 3.70 | 13 547 | 1 841 | 1 152 | |
MGX13 | 0.56 | 35.32 | 304.30 | 7.72 | 80.70 | 2.01 | 1.29 | 14.42 | 173.70 | 5.79 | 13 792 | 4 282 | 1 396 | |
MGX14 | 0.49 | 31.16 | 287.80 | 18.45 | 190.10 | 1.84 | 1.18 | 14.22 | 172.80 | 5.76 | 14 309 | 7 823 | 1 386 | |
玄武岩 | MGX15 | 0.56 | 33.28 | 274.80 | 8.39 | 95.60 | 6.08 | 1.17 | 12.96 | 164.80 | 5.49 | 13 315 | 4 049 | 1 268 |
MGX16 | 0.30 | 29.61 | 828.50 | 21.05 | 412.70 | 3.61 | 3.08 | 40.68 | 245.00 | 5.79 | 20 575 | 10 345 | 1 872 | |
MGX17 | 0.31 | 32.33 | 378.70 | 14.87 | 242.90 | 2.63 | 2.66 | 38.16 | 250.50 | 5.80 | 21 829 | 4 755 | 2 098 | |
MGX18 | 0.24 | 24.96 | 392.00 | 7.09 | 439.70 | 2.00 | 1.90 | 25.58 | 168.00 | 4.68 | 16 670 | 3 760 | 1 287 | |
MGX19 | 0.22 | 23.20 | 495.10 | 12.88 | 235.70 | 3.27 | 2.51 | 34.89 | 170.70 | 4.52 | 15 523 | 6 492 | 1 476 | |
MGX20 | 0.20 | 23.40 | 745.70 | 10.77 | 283.20 | 3.92 | 2.08 | 25.52 | 256.20 | 6.17 | 21 345 | 3 322 | 2 597 | |
MGX21 | 0.28 | 24.93 | 905.90 | 35.09 | 73.62 | 3.78 | 1.67 | 22.11 | 199.20 | 5.95 | 17 163 | 7 746 | 1 759 |
表2 柏木峡—门岗峡蛇绿岩岩石主量(%)、微量(10-6)和稀土元素(10-6)分析结果
Table 2 Analysis results of major(%), trace(10-6)and rare earth elements(10-6) in ophiolite rocks from Baimuxia-Mengangxia area
岩性 | 样品号 | SiO2 | TiO2 | Al2O3 | Fe2O3 | FeO | MnO | MgO | CaO | Na2O | K2O | P2O5 | 烧失量 | 总量 |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
橄榄岩 | MGX01 | 35.07 | 0.07 | 1.17 | 5.46 | 3.27 | 0.12 | 28.90 | 8.68 | 0.02 | 0.03 | 0.02 | 16.08 | 98.89 |
MGX02 | 40.61 | 0.10 | 1.06 | 5.63 | 3.45 | 0.13 | 34.35 | 2.27 | 0.01 | 0.03 | 0.05 | 12.09 | 99.78 | |
MGX03 | 38.85 | 0.06 | 2.40 | 7.53 | 1.30 | 0.12 | 36.92 | 0.23 | 0.32 | 0.03 | 0.04 | 11.91 | 99.73 | |
辉长岩 | MGX04 | 46.16 | 0.34 | 15.51 | 1.35 | 5.08 | 0.10 | 11.18 | 14.27 | 0.81 | 0.10 | 0.05 | 4.88 | 99.83 |
MGX05 | 49.76 | 0.31 | 15.12 | 1.12 | 6.40 | 0.14 | 10.55 | 10.25 | 2.09 | 0.99 | 0.07 | 2.83 | 99.63 | |
MGX06 | 48.71 | 0.57 | 17.42 | 0.70 | 5.70 | 0.11 | 9.06 | 11.30 | 2.15 | 0.83 | 0.07 | 3.22 | 99.84 | |
MGX07 | 49.42 | 0.69 | 13.85 | 2.12 | 8.10 | 0.18 | 8.91 | 11.20 | 2.16 | 0.77 | 0.04 | 2.05 | 99.49 | |
MGX08 | 48.68 | 1.58 | 13.76 | 2.21 | 8.70 | 0.18 | 5.56 | 9.11 | 4.28 | 0.34 | 0.23 | 5.07 | 99.70 | |
MGX09 | 48.09 | 1.72 | 15.47 | 4.38 | 7.40 | 0.24 | 5.38 | 8.87 | 3.31 | 0.82 | 0.26 | 3.70 | 99.64 | |
MGX10 | 46.88 | 2.69 | 13.28 | 3.32 | 10.25 | 0.21 | 6.26 | 11.13 | 2.26 | 0.33 | 0.15 | 2.90 | 99.66 | |
MGX11 | 46.67 | 2.58 | 13.61 | 3.85 | 10.20 | 0.22 | 6.37 | 10.44 | 2.62 | 0.35 | 0.29 | 2.43 | 99.63 | |
MGX12 | 45.37 | 2.14 | 13.75 | 4.39 | 8.05 | 0.18 | 5.68 | 12.72 | 1.96 | 0.21 | 0.25 | 4.76 | 99.46 | |
MGX13 | 49.52 | 2.23 | 13.02 | 3.77 | 8.80 | 0.19 | 5.25 | 9.92 | 3.42 | 0.50 | 0.31 | 2.70 | 99.63 | |
MGX14 | 48.25 | 2.33 | 13.81 | 3.85 | 9.05 | 0.20 | 5.93 | 9.62 | 3.35 | 0.92 | 0.31 | 2.06 | 99.68 | |
玄武岩 | MGX15 | 49.74 | 2.14 | 13.25 | 3.25 | 8.90 | 0.17 | 5.07 | 9.67 | 3.41 | 0.47 | 0.28 | 2.93 | 99.28 |
MGX16 | 46.92 | 3.36 | 15.79 | 3.05 | 10.25 | 0.11 | 6.01 | 8.04 | 2.73 | 1.22 | 0.42 | 1.77 | 99.67 | |
MGX17 | 50.21 | 3.56 | 15.12 | 2.79 | 10.65 | 0.15 | 4.31 | 7.71 | 2.24 | 0.56 | 0.47 | 2.13 | 99.90 | |
MGX18 | 50.10 | 2.64 | 16.55 | 2.07 | 9.15 | 0.12 | 4.85 | 5.92 | 2.83 | 0.43 | 0.28 | 4.74 | 99.68 | |
MGX19 | 48.18 | 2.45 | 14.97 | 6.17 | 4.83 | 0.12 | 6.66 | 8.32 | 1.86 | 0.74 | 0.32 | 5.14 | 99.76 | |
MGX20 | 47.30 | 3.47 | 14.94 | 8.45 | 4.35 | 0.20 | 7.57 | 8.12 | 2.09 | 0.39 | 0.58 | 2.42 | 99.88 | |
MGX21 | 45.75 | 2.70 | 14.86 | 5.94 | 7.40 | 0.22 | 8.67 | 7.23 | 0.28 | 0.88 | 0.38 | 5.45 | 99.76 | |
岩性 | 样品号 | La | Ce | Pr | Nd | Sm | Eu | Gd | Tb | Dy | Ho | Er | Tm | Yb |
橄榄岩 | MGX01 | 2.00 | 3.22 | 0.44 | 1.71 | 0.28 | 0.17 | 0.28 | 0.05 | 0.25 | 0.05 | 0.13 | 0.02 | 0.14 |
MGX02 | 2.17 | 5.87 | 0.82 | 3.76 | 0.82 | 0.25 | 0.64 | 0.07 | 0.41 | 0.07 | 0.18 | 0.02 | 0.15 | |
MGX03 | 2.04 | 3.79 | 0.57 | 2.21 | 0.44 | 0.11 | 0.50 | 0.09 | 0.61 | 0.13 | 0.37 | 0.06 | 0.46 | |
辉长岩 | MGX04 | 2.91 | 6.73 | 0.80 | 4.58 | 1.22 | 0.47 | 1.21 | 0.18 | 1.13 | 0.23 | 0.60 | 0.08 | 0.53 |
MGX05 | 5.91 | 11.88 | 1.48 | 6.06 | 1.33 | 0.51 | 1.60 | 0.31 | 2.01 | 0.43 | 1.22 | 0.21 | 1.38 | |
MGX06 | 1.96 | 5.12 | 0.83 | 4.07 | 1.37 | 0.61 | 1.76 | 0.31 | 2.18 | 0.41 | 1.16 | 0.18 | 1.14 | |
MGX07 | 3.79 | 6.51 | 0.84 | 3.76 | 1.17 | 0.60 | 1.61 | 0.33 | 2.14 | 0.46 | 1.32 | 0.22 | 1.45 | |
MGX08 | 11.91 | 26.24 | 4.17 | 19.61 | 4.76 | 1.48 | 5.57 | 1.04 | 6.51 | 1.34 | 3.85 | 0.63 | 4.10 | |
MGX09 | 11.18 | 25.03 | 3.63 | 17.47 | 4.69 | 1.51 | 5.31 | 0.97 | 6.13 | 1.24 | 3.61 | 0.59 | 3.57 | |
MGX10 | 8.02 | 18.98 | 2.93 | 14.04 | 4.09 | 1.34 | 4.40 | 0.81 | 5.15 | 1.06 | 2.98 | 0.47 | 2.88 | |
MGX11 | 11.47 | 29.09 | 4.64 | 22.80 | 6.49 | 2.07 | 7.01 | 1.32 | 7.99 | 1.59 | 4.60 | 0.71 | 4.38 | |
MGX12 | 10.01 | 25.00 | 3.81 | 18.16 | 4.81 | 1.63 | 5.05 | 0.90 | 5.35 | 1.03 | 2.84 | 0.42 | 2.66 | |
MGX13 | 17.17 | 37.04 | 5.57 | 25.68 | 6.18 | 2.14 | 6.71 | 1.21 | 6.99 | 1.40 | 3.78 | 0.61 | 3.86 | |
MGX14 | 17.44 | 38.94 | 5.58 | 25.28 | 5.81 | 2.19 | 6.47 | 1.11 | 6.47 | 1.26 | 3.30 | 0.55 | 3.38 | |
玄武岩 | MGX15 | 13.67 | 30.34 | 4.67 | 22.00 | 5.37 | 1.87 | 6.26 | 1.13 | 6.74 | 1.35 | 3.63 | 0.59 | 3.81 |
MGX16 | 32.20 | 63.91 | 8.43 | 36.29 | 8.02 | 2.58 | 7.26 | 1.15 | 6.23 | 1.08 | 2.82 | 0.39 | 2.35 | |
MGX17 | 28.22 | 57.93 | 7.81 | 34.83 | 8.23 | 2.63 | 7.63 | 1.30 | 6.99 | 1.23 | 3.11 | 0.44 | 2.48 | |
MGX18 | 19.86 | 40.81 | 5.48 | 24.71 | 6.17 | 2.11 | 6.21 | 1.04 | 5.59 | 1.00 | 2.4 | 0.35 | 1.93 | |
MGX19 | 22.77 | 43.96 | 5.63 | 24.46 | 5.82 | 1.79 | 5.53 | 0.89 | 4.93 | 0.88 | 2.29 | 0.32 | 1.75 | |
MGX20 | 34.71 | 72.39 | 9.50 | 41.05 | 9.00 | 2.95 | 7.43 | 1.11 | 5.42 | 0.91 | 2.10 | 0.28 | 1.56 | |
MGX21 | 22.79 | 49.71 | 6.60 | 28.82 | 6.53 | 2.18 | 6.62 | 0.99 | 5.39 | 0.98 | 2.45 | 0.33 | 2.00 | |
岩性 | 样品号 | Lu | Y | Sr | Rb | Ba | Th | Ta | Nb | Zr | Hf | Ti | K | P |
橄榄岩 | MGX01 | 0.02 | 1.39 | 63.50 | 1.83 | 206.70 | 0.44 | 0.07 | 0.46 | 6.80 | 0.18 | 507 | 301 | 105 |
MGX02 | 0.02 | 2.05 | 12.84 | 0.63 | 68.77 | 0.31 | 0.26 | 0.66 | 12.79 | 0.47 | 684 | 284 | 249 | |
MGX03 | 0.07 | 3.36 | 12.60 | 2.97 | 8.90 | 1.10 | 0.10 | 0.80 | 9.60 | 0.32 | 410 | 284 | 199 | |
辉长岩 | MGX04 | 0.07 | 5.66 | 395.50 | 1.55 | 47.94 | 0.37 | 0.33 | 0.85 | 15.06 | 0.63 | 2 147 | 874 | 230 |
MGX05 | 0.21 | 10.74 | 298.70 | 37.78 | 191.70 | 2.36 | 0.24 | 2.02 | 24.00 | 0.80 | 1 920 | 8 490 | 316 | |
MGX06 | 0.15 | 11.31 | 275.50 | 30.32 | 122.60 | 1.29 | 0.39 | 2.05 | 32.78 | 1.27 | 3 537 | 7 131 | 316 | |
MGX07 | 0.21 | 11.21 | 182.00 | 2.39 | 194.10 | 0.85 | 0.29 | 1.28 | 19.40 | 0.65 | 4 245 | 6 560 | 179 | |
MGX08 | 0.60 | 33.59 | 204.50 | 5.84 | 82.80 | 1.04 | 0.73 | 8.95 | 156.20 | 5.21 | 10 010 | 2 983 | 1 061 | |
MGX09 | 0.54 | 33.12 | 427.40 | 10.69 | 355.50 | 0.17 | 0.93 | 12.74 | 128.50 | 3.71 | 10 748 | 7 095 | 1 183 | |
MGX10 | 0.41 | 28.61 | 225.70 | 5.95 | 136.10 | 0.61 | 0.60 | 7.85 | 107.00 | 2.96 | 16 667 | 2 831 | 677 | |
MGX11 | 0.63 | 42.66 | 251.40 | 2.95 | 166.40 | 0.38 | 0.93 | 11.80 | 167.00 | 5.75 | 15 913 | 2 989 | 1 302 | |
MGX12 | 0.37 | 27.38 | 465.70 | 1.34 | 152.70 | 0.13 | 0.94 | 13.62 | 126.60 | 3.70 | 13 547 | 1 841 | 1 152 | |
MGX13 | 0.56 | 35.32 | 304.30 | 7.72 | 80.70 | 2.01 | 1.29 | 14.42 | 173.70 | 5.79 | 13 792 | 4 282 | 1 396 | |
MGX14 | 0.49 | 31.16 | 287.80 | 18.45 | 190.10 | 1.84 | 1.18 | 14.22 | 172.80 | 5.76 | 14 309 | 7 823 | 1 386 | |
玄武岩 | MGX15 | 0.56 | 33.28 | 274.80 | 8.39 | 95.60 | 6.08 | 1.17 | 12.96 | 164.80 | 5.49 | 13 315 | 4 049 | 1 268 |
MGX16 | 0.30 | 29.61 | 828.50 | 21.05 | 412.70 | 3.61 | 3.08 | 40.68 | 245.00 | 5.79 | 20 575 | 10 345 | 1 872 | |
MGX17 | 0.31 | 32.33 | 378.70 | 14.87 | 242.90 | 2.63 | 2.66 | 38.16 | 250.50 | 5.80 | 21 829 | 4 755 | 2 098 | |
MGX18 | 0.24 | 24.96 | 392.00 | 7.09 | 439.70 | 2.00 | 1.90 | 25.58 | 168.00 | 4.68 | 16 670 | 3 760 | 1 287 | |
MGX19 | 0.22 | 23.20 | 495.10 | 12.88 | 235.70 | 3.27 | 2.51 | 34.89 | 170.70 | 4.52 | 15 523 | 6 492 | 1 476 | |
MGX20 | 0.20 | 23.40 | 745.70 | 10.77 | 283.20 | 3.92 | 2.08 | 25.52 | 256.20 | 6.17 | 21 345 | 3 322 | 2 597 | |
MGX21 | 0.28 | 24.93 | 905.90 | 35.09 | 73.62 | 3.78 | 1.67 | 22.11 | 199.20 | 5.95 | 17 163 | 7 746 | 1 759 |
图7 柏木峡—门岗峡蛇绿岩ACM((a),底图据文献[33])和SiO2-FeOt/MgO((b),底图据文献[34])图解
Fig.7 ACM(a) and SiO2-FeOt/MgO(b) diagrams of the Baimuxia-Mengangxia ophiolite(base map after refs.[33]and[34], respectively)
图8 柏木峡—门岗峡蛇绿岩稀土元素球粒陨石标准化配分图和微量元素原始地幔标准经蛛网图(底图据文献[35])
Fig.8 Chondrite-normalized REE patterns and spidergrams of trace elements of the Baimuxia-Mengangxia ophiolite(base map after ref.[35])
图9 柏木峡—门岗峡蛇绿岩构造环境判别图解 (a)Nb-Zr-Y图解,底图据文献[37];(b)Hf-Th-Ta图解,底图据文献[38];(c)TiO2-MnO-P2O5图解,底图据文献[39];(d)TiO2-FeO*/MgO图解,底图据文献[40];(e) Nb/Yb-Th/Yb图解,底图据文献[36];(f)Nb/Yb-TiO2/Yb图解,底图据文献[41];AI.板内碱性玄武岩;AⅡ.板内拉斑玄武岩;N-MORB/MORB.洋中脊玄武岩;E-MORB.富集型洋中脊玄武岩;WPB.板内玄武岩;WPA.板内碱性玄武岩;IAT.岛弧拉斑玄武岩;CABI.岛弧钙碱性玄武岩;OIT.洋岛拉斑玄武岩;OIA.洋岛碱性玄武岩;CAB.钙碱性玄武岩
Fig.9 Tectonic discrimination diagrams of Baimuxia-Mengangxia ophiolite
[1] | 周国庆. 蛇绿岩研究新进展及其定义和分类的再讨论[J]. 南京大学学报(自然科学版), 2008, 44(1):1-24. |
[2] | 张旗. 蛇绿岩的分类[J]. 地质科学, 1990, 25(1):54-61. |
[3] | 史仁灯. 蛇绿岩研究进展、存在问题及思考[J]. 地质论评, 2005, 51(6):681-693. |
[4] | 张达, 吴淦国. 第32届国际地质大会造山带和蛇绿岩研究进展[J]. 现代地质, 2004, 18(4):443-448. |
[5] | 臧遇时, 杨高学, 赵金凤. 蛇绿岩的定义、分类及其发展[J]. 西北地质, 2013, 46(2):12-17. |
[6] | 张旗, 肖序常. 中国蛇绿岩研究概述[J]. 岩石学报, 1995, 11(增刊):1-9. |
[7] |
DILEK Y, FURNES H. Ophiolite genesis and global tectonics:Geochemical and tectonic fingerprinting of ancient oceanic lithosphere[J]. Geological Society of America Bulletin, 2011, 123(3/4):387-411.
DOI URL |
[8] | 张进, 邓晋福, 肖庆辉, 等. 蛇绿岩研究的最新进展[J]. 地质通报, 2012, 31(1):1-12. |
[9] | 黄汲清, 任纪舜, 姜春发, 等. 中国大地构造基本轮廓[J]. 地质学报, 1977, 51(2):117-135. |
[10] | 肖序常, 陈国铭, 朱志直. 祁连山古板块构造的一些认识[J]. 地质科技, 1974(3):73-78. |
[11] | 冯益民, 何世平. 祁连山大地构造与造山作用[M]. 北京: 地质出版社, 1996. |
[12] | 冯益民, 何世平. 蛇绿岩与造山作用--北祁连造山带例析[M]//张旗. 蛇绿岩与地球动力学研究. 北京: 地质出版社, 1996:135-138. |
[13] | 王荃, 刘雪亚. 我国西部祁连山区的古海洋地壳及其大地构造意义[J]. 地质科学, 1976, 11(1):42-55. |
[14] | 肖序常, 陈国铭, 朱志直. 祁连山古蛇绿岩带的地质构造意义[J]. 地质学报, 1978, 52(4):281-295. |
[15] | 冯益民, 何世平. 北祁连山蛇绿岩地质和地球化学研究[J]. 岩石学报, 1995, 11(增刊):125-146. |
[16] | 张旗, 孙晓猛, 周德进, 等. 北祁连蛇绿岩的特征、形成环境及其构造意义[J]. 地球科学进展, 1997, 12(4):366-393. |
[17] | 钱青, 张旗, 孙晓猛. 北祁连九个泉玄武岩的形成环境及地幔源区特征:微量元素和Nd同位素地球化学制约[J]. 岩石学报, 2001, 17(3):385-394. |
[18] | 武鹏, 李向民, 徐学义, 等. 北祁连山扎麻什地区东沟蛇绿岩LA-ICP-MS锆石U-Pb测年及其地球化学特征[J]. 地质通报, 2012, 31(6):896-906. |
[19] | 夏小洪, 宋述光. 北祁连山肃南九个泉蛇绿岩形成年龄和构造环境[J]. 科学通报, 2010, 55(15):1465-1473. |
[20] | 史仁灯, 杨经绥, 吴才来, 等. 北祁连玉石沟蛇绿岩形成于晚震旦世的SHRIMP年龄证据[J]. 地质学报, 2004, 78(5):649-657. |
[21] | 侯青叶, 赵志丹, 张宏飞, 等. 北祁连玉石沟蛇绿岩印度洋MORB型同位素组成特征及其地质意义[J]. 中国科学(D辑:地球科学), 2005, 35(8):710-719. |
[22] | 夏小洪, 孙楠, 宋述光, 等. 北祁连西段熬油沟-二只哈拉达坂蛇绿岩的形成环境和时代[J]. 北京大学学报(自然科学版), 2012, 48(5):757-769. |
[23] | 相振群, 陆松年, 李怀坤, 等. 北祁连西段熬油沟辉长岩的锆石SHRIMP U-Pb年龄及地质意义[J]. 地质通报, 2007, 26(12):1686-1691. |
[24] | 张招崇, 毛景文, 左国朝, 等. 北祁连西段熬油沟蛇绿岩岩石成因的矿物学研究[J]. 矿物学报, 1999, 19(1):77-82. |
[25] | 张招崇, 周美付, ROBINSON P T, 等. 北祁连山西段熬油沟蛇绿岩SHRIMP分析结果及其地质意义[J]. 岩石学报, 2001, 17(2):222-226. |
[26] | 曾建元, 杨怀仁, 杨宏仪, 等. 北祁连东草河蛇绿岩:一个早古生代的洋壳残片[J]. 科学通报, 2007, 52(7):825-835. |
[27] | 夏林圻, 夏祖春, 徐学义, 等. 北祁连海相火山岩岩石成因[M]. 北京: 地质出版社, 1996. |
[28] |
SONG S G, SU L, NIU Y L, et al. CH4 inclusions in orogenic harzburgite:Evidence for reduced slab fluids and implication for redox melting in mantle wedge[J]. Geochimica et Cosmochimica Acta, 2009, 73(6):1737-1754.
DOI URL |
[29] | 王永和, 焦养泉, 李建星, 等. 中祁连北缘奥陶纪岩浆弧地层[J]. 现代地质, 2008, 22(5):724-732. |
[30] | 李冰, 胡道功, 陈宣华, 等. 北祁连缝合带油葫芦沟蛇绿岩中花岗斑岩锆石U-Pb年龄及地质意义[J]. 现代地质, 2017, 31(6):1170-1176. |
[31] | 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(增刊):600-601. |
[32] | 吴元保, 郑永飞. 锆石成因矿物学研究及其对U-Pb年龄解释的制约[J]. 科学通报, 2004, 49(16):1589-1604. |
[33] |
COLEMAN M L. Sulphur isotopes in petrology[J]. Journal of the Geological Society, 1977, 133(6):593-608.
DOI URL |
[34] |
MIYASHIRO A. Classification,characteristics and origin of ophiolites[J]. Journal of Geology, 1975, 83:249-281.
DOI URL |
[35] |
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 |
[36] |
PEARCE J A. Geochemical fingerprinting of oceanic basalts with applications to ophiolite classification and the search for Archean oceanic crust[J]. Lithos, 2008, 100(1/2/3/4):14-48.
DOI URL |
[37] |
MESCHEDE MA. method of discriminating between different types of mid-ocean ridge basalts and continental tholeiites with the Nb-Zr-Y diagram[J]. Chemical Geology, 1986, 56:207-218.
DOI URL |
[38] |
WOOD D A. The application of a Th-Hf-Ta diagram to problems of tectonomagmatic classification and to establishing the nature of crustal contamination of basaltic lavas of the British Tertiary Volcanic Province[J]. Earth and Planetary Science Letters, 1980, 50(1):11-30.
DOI URL |
[39] |
MULLEN E D. MnO/TiO2/P2O5:a minor element discriminant for basaltic rocks of oceanic environments and its implications for petrogenesis[J]. Earth and Planetary Science Letters, 1983, 62:53-62.
DOI URL |
[40] | PEARCE J A. Trace element characteristics of lavas from destructive plate boundaries[M]// THORPE R S. Andesites:Orogenic Andesites and Related Rocks. New York: Jehn Wiley and Sons, 1982: 525-548. |
[41] |
PEARCE J A. Immobile element fingerprinting of ophiolites[J]. Elements, 2014, 10(2):101-108.
DOI URL |
[42] | 刘宝山, 蔡进福, 雷晓清, 等. 北祁连玉龙滩地区寒武纪花岗岩地质地球化学特征[J]. 西北地质, 2016, 49(4):43-50. |
[43] | 王国良, 叶占福, 祁生胜, 等. 北祁连龙王山晚志留世花岗岩LA-ICP-MS锆石U-Pb测年及其地球化学特征[J]. 矿产与地质, 2013, 27(6):462-470. |
[1] | 宋志杰, 刘文灿, 张宏远, 柳长峰, 罗凯, 吴晨. 祁连山西段玉石沟地区上二叠统砂岩碎屑锆石年代学及其地质意义[J]. 现代地质, 2019, 33(01): 112-120. |
[2] | 袁建国, 任永健, 姜振宁, 屈云燕, 魏浩. 内蒙古锡林浩特毛登牧场早石炭世花岗岩锆石U-Pb年龄、地球化学特征及其地质意义[J]. 现代地质, 2017, 31(06): 1131-1146. |
[3] | 张承帅, 李莉, 张长青, 王九如. 福建龙岩大洋花岗岩LA-ICP-MS锆石U-Pb测年、Hf同位素组成及其地质意义[J]. 现代地质, 2012, 26(3): 433-444. |
阅读次数 | ||||||
全文 |
|
|||||
摘要 |
|
|||||