Geoscience ›› 2022, Vol. 36 ›› Issue (03): 824-835.DOI: 10.19657/j.geoscience.1000-8527.2022.013
• Petrology • Previous Articles Next Articles
YANG Hanwen1,2(), WANG Jianzhong3,4(), ZHAO Jun4,5, DUAN Jun3, WANG Rongmin6, GAO Wenbin3, WEI Wenhao1, ZHENG Yanhe1
Received:
2021-01-17
Revised:
2022-04-30
Online:
2022-06-10
Published:
2022-07-19
Contact:
WANG Jianzhong
CLC Number:
YANG Hanwen, WANG Jianzhong, ZHAO Jun, DUAN Jun, WANG Rongmin, GAO Wenbin, WEI Wenhao, ZHENG Yanhe. Ancient Crust Remelting in Wenquan Area, Xinjiang: Evidence from the Age and Sr-Nd Isotopes of the Late Carboniferous Granite Porphyry Dykes[J]. Geoscience, 2022, 36(03): 824-835.
测点 | Pb /10-6 | 232Th /10-6 | 238U /10-6 | Th/U | 同位素比值 | 同位素年龄/Ma | 不谐 和度 /% | |||||
---|---|---|---|---|---|---|---|---|---|---|---|---|
207Pb/206Pb ±1σ | 207Pb/235U ±1σ | 206Pb/238U ±1σ | ||||||||||
207Pb/206Pb ±1σ | 207Pb/235U ±1σ | 206Pb/238U ±1σ | ||||||||||
1 | 72 | 411 | 1 186 | 0.35 | 0.052 2±0.002 9 | 0.380 0±0.020 7 | 0.052 8±0.000 9 | 294±122 | 327±15 | 331.4±5.4 | -1.3 | |
6 | 76 | 469 | 1 365 | 0.34 | 0.054 3±0.002 2 | 0.366 3±0.014 7 | 0.048 8±0.000 7 | 385±88 | 317±11 | 307.3±4.4 | 3.0 | |
7 | 61 | 440 | 1 074 | 0.41 | 0.052 3±0.002 4 | 0.346 7±0.015 6 | 0.048 0±0.000 7 | 299±101 | 302±12 | 302.3±4.5 | 0.0 | |
8 | 107 | 1 567 | 1 176 | 1.33 | 0.051 4±0.002 5 | 0.454 4±0.021 8 | 0.064 1±0.001 0 | 259±108 | 380±15 | 400.2±5.8 | -5.2 | |
10 | 50 | 162 | 928 | 0.17 | 0.051 9±0.002 4 | 0.352 2±0.016 3 | 0.049 2±0.000 8 | 281±104 | 306±12 | 309.4±4.7 | -1.0 | |
11 | 92 | 500 | 1 708 | 0.29 | 0.052 2±0.001 8 | 0.339 9±0.011 4 | 0.047 1±0.000 6 | 296±75 | 297±9 | 296.9±4.0 | 0.1 | |
12 | 70 | 393 | 1 259 | 0.31 | 0.051 9±0.002 1 | 0.346 3±0.013 8 | 0.048 4±0.000 7 | 279±89 | 302±10 | 304.5±4.3 | -0.9 | |
13 | 16 | 101 | 289 | 0.35 | 0.051 0±0.004 5 | 0.344 2±0.030 1 | 0.048 9±0.001 0 | 242±192 | 300±23 | 307.5±6.3 | -2.4 | |
14 | 36 | 286 | 661 | 0.43 | 0.049 2±0.002 7 | 0.315 2±0.017 1 | 0.046 4±0.000 8 | 158±124 | 278±13 | 292.2±4.7 | -5.0 | |
15 | 43 | 255 | 555 | 0.46 | 0.055 6±0.002 8 | 0.502 9±0.024 7 | 0.065 5±0.001 1 | 437±108 | 414±17 | 408.9±6.4 | 1.2 | |
16 | 83 | 443 | 1 502 | 0.29 | 0.053 2±0.001 8 | 0.358 1±0.012 0 | 0.048 7±0.000 7 | 338±75 | 311±9 | 306.7±4.1 | 1.3 | |
17 | 41 | 250 | 474 | 0.53 | 0.055 4±0.002 8 | 0.539 4±0.026 7 | 0.070 5±0.001 1 | 429±108 | 438±18 | 439.0±6.9 | -0.2 | |
18 | 57 | 378 | 571 | 0.66 | 0.064 1±0.002 8 | 0.700 3±0.030 3 | 0.079 1±0.001 2 | 745±90 | 539±18 | 490.9±7.3 | 8.9 | |
20 | 83 | 334 | 1 652 | 0.20 | 0.054 3±0.0024 | 0.337 6±0.014 6 | 0.045 0±0.000 7 | 383±96 | 295±11 | 283.9±4.3 | 3.9 | |
21 | 56 | 361 | 885 | 0.41 | 0.052 4±0.002 2 | 0.393 1±0.016 0 | 0.054 3±0.000 8 | 304±91 | 337±12 | 340.7±4.8 | -1.2 | |
22 | 129 | 161 | 2 383 | 0.07 | 0.052 4±0.001 4 | 0.365 8±0.009 9 | 0.050 6±0.000 7 | 302±60 | 317±7 | 318.0±4.0 | -0.4 | |
23 | 61 | 31 | 1 153 | 0.03 | 0.051 4±0.002 0 | 0.356 6±0.013 5 | 0.050 2±0.000 7 | 258±85 | 310±10 | 316.0±4.3 | -2.0 | |
24 | 65 | 571 | 790 | 0.72 | 0.055 4±0.002 2 | 0.485 5±0.019 1 | 0.063 5±0.000 9 | 428±86 | 402±13 | 396.6±5.6 | 1.3 | |
25 | 33 | 81 | 566 | 0.14 | 0.056 6±0.003 1 | 0.401 2±0.021 8 | 0.051 4±0.000 9 | 473±118 | 343±16 | 322.9±5.3 | 5.7 | |
26 | 63 | 610 | 1 024 | 0.60 | 0.053 0±0.002 1 | 0.361 9±0.014 2 | 0.049 5±0.000 7 | 327±88 | 314±11 | 311.2±4.4 | 0.8 | |
29 | 74 | 412 | 1 278 | 0.32 | 0.059 1±0.002 1 | 0.402 7±0.013 9 | 0.049 3±0.000 7 | 572±74 | 344±10 | 310.1±4.2 | 9.7 | |
30 | 52 | 303 | 964 | 0.31 | 0.052 7±0.002 2 | 0.343 5±0.014 2 | 0.047 2±0.000 7 | 315±92 | 300±11 | 297.3±4.2 | 0.9 | |
31 | 164 | 1 111 | 2 211 | 0.50 | 0.055 6±0.001 3 | 0.472 5±0.011 2 | 0.061 5±0.000 8 | 435±52 | 393±8 | 384.9±4.7 | 2.0 | |
32 | 109 | 301 | 1 939 | 0.16 | 0.051 6±0.001 4 | 0.369 0±0.010 1 | 0.051 7±0.000 7 | 270±62 | 319±8 | 325.0±4.1 | -1.9 | |
33 | 62 | 354 | 1 086 | 0.33 | 0.051 4±0.001 9 | 0.349 3±0.013 0 | 0.049 1±0.000 7 | 261±84 | 304±10 | 309.2±4.2 | -1.6 | |
35 | 61 | 270 | 1 044 | 0.26 | 0.054 6±0.002 0 | 0.388 6±0.014 2 | 0.051 5±0.000 7 | 396±80 | 333±10 | 323.7±4.5 | 2.9 |
Table 1 Zircon U-Pb dating data of the Wenquan granite porphyry dykes
测点 | Pb /10-6 | 232Th /10-6 | 238U /10-6 | Th/U | 同位素比值 | 同位素年龄/Ma | 不谐 和度 /% | |||||
---|---|---|---|---|---|---|---|---|---|---|---|---|
207Pb/206Pb ±1σ | 207Pb/235U ±1σ | 206Pb/238U ±1σ | ||||||||||
207Pb/206Pb ±1σ | 207Pb/235U ±1σ | 206Pb/238U ±1σ | ||||||||||
1 | 72 | 411 | 1 186 | 0.35 | 0.052 2±0.002 9 | 0.380 0±0.020 7 | 0.052 8±0.000 9 | 294±122 | 327±15 | 331.4±5.4 | -1.3 | |
6 | 76 | 469 | 1 365 | 0.34 | 0.054 3±0.002 2 | 0.366 3±0.014 7 | 0.048 8±0.000 7 | 385±88 | 317±11 | 307.3±4.4 | 3.0 | |
7 | 61 | 440 | 1 074 | 0.41 | 0.052 3±0.002 4 | 0.346 7±0.015 6 | 0.048 0±0.000 7 | 299±101 | 302±12 | 302.3±4.5 | 0.0 | |
8 | 107 | 1 567 | 1 176 | 1.33 | 0.051 4±0.002 5 | 0.454 4±0.021 8 | 0.064 1±0.001 0 | 259±108 | 380±15 | 400.2±5.8 | -5.2 | |
10 | 50 | 162 | 928 | 0.17 | 0.051 9±0.002 4 | 0.352 2±0.016 3 | 0.049 2±0.000 8 | 281±104 | 306±12 | 309.4±4.7 | -1.0 | |
11 | 92 | 500 | 1 708 | 0.29 | 0.052 2±0.001 8 | 0.339 9±0.011 4 | 0.047 1±0.000 6 | 296±75 | 297±9 | 296.9±4.0 | 0.1 | |
12 | 70 | 393 | 1 259 | 0.31 | 0.051 9±0.002 1 | 0.346 3±0.013 8 | 0.048 4±0.000 7 | 279±89 | 302±10 | 304.5±4.3 | -0.9 | |
13 | 16 | 101 | 289 | 0.35 | 0.051 0±0.004 5 | 0.344 2±0.030 1 | 0.048 9±0.001 0 | 242±192 | 300±23 | 307.5±6.3 | -2.4 | |
14 | 36 | 286 | 661 | 0.43 | 0.049 2±0.002 7 | 0.315 2±0.017 1 | 0.046 4±0.000 8 | 158±124 | 278±13 | 292.2±4.7 | -5.0 | |
15 | 43 | 255 | 555 | 0.46 | 0.055 6±0.002 8 | 0.502 9±0.024 7 | 0.065 5±0.001 1 | 437±108 | 414±17 | 408.9±6.4 | 1.2 | |
16 | 83 | 443 | 1 502 | 0.29 | 0.053 2±0.001 8 | 0.358 1±0.012 0 | 0.048 7±0.000 7 | 338±75 | 311±9 | 306.7±4.1 | 1.3 | |
17 | 41 | 250 | 474 | 0.53 | 0.055 4±0.002 8 | 0.539 4±0.026 7 | 0.070 5±0.001 1 | 429±108 | 438±18 | 439.0±6.9 | -0.2 | |
18 | 57 | 378 | 571 | 0.66 | 0.064 1±0.002 8 | 0.700 3±0.030 3 | 0.079 1±0.001 2 | 745±90 | 539±18 | 490.9±7.3 | 8.9 | |
20 | 83 | 334 | 1 652 | 0.20 | 0.054 3±0.0024 | 0.337 6±0.014 6 | 0.045 0±0.000 7 | 383±96 | 295±11 | 283.9±4.3 | 3.9 | |
21 | 56 | 361 | 885 | 0.41 | 0.052 4±0.002 2 | 0.393 1±0.016 0 | 0.054 3±0.000 8 | 304±91 | 337±12 | 340.7±4.8 | -1.2 | |
22 | 129 | 161 | 2 383 | 0.07 | 0.052 4±0.001 4 | 0.365 8±0.009 9 | 0.050 6±0.000 7 | 302±60 | 317±7 | 318.0±4.0 | -0.4 | |
23 | 61 | 31 | 1 153 | 0.03 | 0.051 4±0.002 0 | 0.356 6±0.013 5 | 0.050 2±0.000 7 | 258±85 | 310±10 | 316.0±4.3 | -2.0 | |
24 | 65 | 571 | 790 | 0.72 | 0.055 4±0.002 2 | 0.485 5±0.019 1 | 0.063 5±0.000 9 | 428±86 | 402±13 | 396.6±5.6 | 1.3 | |
25 | 33 | 81 | 566 | 0.14 | 0.056 6±0.003 1 | 0.401 2±0.021 8 | 0.051 4±0.000 9 | 473±118 | 343±16 | 322.9±5.3 | 5.7 | |
26 | 63 | 610 | 1 024 | 0.60 | 0.053 0±0.002 1 | 0.361 9±0.014 2 | 0.049 5±0.000 7 | 327±88 | 314±11 | 311.2±4.4 | 0.8 | |
29 | 74 | 412 | 1 278 | 0.32 | 0.059 1±0.002 1 | 0.402 7±0.013 9 | 0.049 3±0.000 7 | 572±74 | 344±10 | 310.1±4.2 | 9.7 | |
30 | 52 | 303 | 964 | 0.31 | 0.052 7±0.002 2 | 0.343 5±0.014 2 | 0.047 2±0.000 7 | 315±92 | 300±11 | 297.3±4.2 | 0.9 | |
31 | 164 | 1 111 | 2 211 | 0.50 | 0.055 6±0.001 3 | 0.472 5±0.011 2 | 0.061 5±0.000 8 | 435±52 | 393±8 | 384.9±4.7 | 2.0 | |
32 | 109 | 301 | 1 939 | 0.16 | 0.051 6±0.001 4 | 0.369 0±0.010 1 | 0.051 7±0.000 7 | 270±62 | 319±8 | 325.0±4.1 | -1.9 | |
33 | 62 | 354 | 1 086 | 0.33 | 0.051 4±0.001 9 | 0.349 3±0.013 0 | 0.049 1±0.000 7 | 261±84 | 304±10 | 309.2±4.2 | -1.6 | |
35 | 61 | 270 | 1 044 | 0.26 | 0.054 6±0.002 0 | 0.388 6±0.014 2 | 0.051 5±0.000 7 | 396±80 | 333±10 | 323.7±4.5 | 2.9 |
样号 | 87Rb/86Sr | 87Sr/86Sr±2σ | ISr | 147Sm/ 144Nd | 143Nd/144Nd ±2σ | 锆石年龄 /Ma | εNd(0) | εNd(t) | fSm/Nd | TDM1 /Ma | TDMC /Ma |
---|---|---|---|---|---|---|---|---|---|---|---|
PM4-96-YQ1 | 2.083 6 | 0.719 2±17 | 0.710 018 | 0.113 0 | 0.512 3±22 | 310 | -6.67 | -3.36 | -0.43 | 1 294 | 1 345 |
PM4-96-YQ2 | 2.871 6 | 0.722 6±14 | 0.709 966 | 0.127 3 | 0.512 4±12 | 310 | -5.62 | -2.87 | -0.35 | 1 413 | 1 306 |
PM4-96-YQ3 | 2.644 9 | 0.721 6±13 | 0.709 944 | 0.125 0 | 0.512 4±1 | 310 | -5.17 | -2.33 | -0.36 | 1 337 | 1 262 |
PM4-98-YQ1 | 1.863 1 | 0.717 5±14 | 0.709 328 | 0.127 0 | 0.512 3±11 | 310 | -6.67 | -3.92 | -0.35 | 1 502 | 1 390 |
Table 2 Sr-Nd isotope data of the Wenquan granite porphyry
样号 | 87Rb/86Sr | 87Sr/86Sr±2σ | ISr | 147Sm/ 144Nd | 143Nd/144Nd ±2σ | 锆石年龄 /Ma | εNd(0) | εNd(t) | fSm/Nd | TDM1 /Ma | TDMC /Ma |
---|---|---|---|---|---|---|---|---|---|---|---|
PM4-96-YQ1 | 2.083 6 | 0.719 2±17 | 0.710 018 | 0.113 0 | 0.512 3±22 | 310 | -6.67 | -3.36 | -0.43 | 1 294 | 1 345 |
PM4-96-YQ2 | 2.871 6 | 0.722 6±14 | 0.709 966 | 0.127 3 | 0.512 4±12 | 310 | -5.62 | -2.87 | -0.35 | 1 413 | 1 306 |
PM4-96-YQ3 | 2.644 9 | 0.721 6±13 | 0.709 944 | 0.125 0 | 0.512 4±1 | 310 | -5.17 | -2.33 | -0.36 | 1 337 | 1 262 |
PM4-98-YQ1 | 1.863 1 | 0.717 5±14 | 0.709 328 | 0.127 0 | 0.512 3±11 | 310 | -6.67 | -3.92 | -0.35 | 1 502 | 1 390 |
[1] | 张作衡, 王志良, 左国朝. 新疆西天山地质构造演化及铜金多金属矿床成矿环境[M]. 北京: 地质出版社, 2008. |
[2] | 陈江峰, 陈道公, 李学明, 等. 新疆阿拉套花岗岩类K-Ar和40Ar-39Ar同位素定年[J]. 岩石学报, 1994, 10(2):184-192. |
[3] |
CHEN J F, ZHOU T X, XIE Z, et al. Formation of positive εNd(T) granitoids from the Alataw Mountains, Xinjiang, China, by mixing and fractional crystallization: implication for Phanerozoic crustal growth[J]. Tectonophysics, 2000, 328:53-67.
DOI URL |
[4] | 林涛, 邓宇峰, 陈斌, 等. 新疆西天山阿拉套山东部孔吾萨依A型花岗岩成岩年代、地球化学特征及成因[J]. 地质学报, 2019, 93(5):1020-1036. |
[5] | 刘志强, 韩宝福, 季建清, 等. 新疆阿拉套山东部后碰撞岩浆活动的时代、地球化学性质及其对陆垂向增长的意义[J]. 岩石学报, 2005, 21(3):623-639. |
[6] | 陈必河, 罗照华, 贾宝华, 等. 阿拉套山南缘岩浆岩锆石SHRIMP年代学研究[J]. 岩石学报, 2007, 23(7):1756-1764. |
[7] |
WANG Q, DEREK A W, ZHAO Z H, et al. Petrogenesis of Carboniferous adakites and Nb-enriched arc basalts in the Alataw area, northern Tianshan Range (western China): Implications for Phanerozoic crustal growth in the Central Asia orogenic belt[J]. Chemical Geology, 2007, 236:42-64.
DOI URL |
[8] | 江秀敏. 新疆阿拉套山东段晚古生代侵入岩活动特征及其成矿意义[D]. 北京: 中国地质大学, 2015:1-47. |
[9] | 王建中, 赵军, 段俊. 西天山察哈乌苏侵入体LA-ICP-MS锆石U-Pb年龄、Hf同位素特征及其地质意义[J]. 世界地质, 2021, 40(3):560-575. |
[10] | 王建中, 魏立勇, 段俊, 等. 新疆阿拉套山西段察哈乌苏二长花岗岩成因及构造意义[J]. 西北地质, 2021, 54(3):10-26. |
[11] | 江秀敏, 罗照华, 陈必河, 等. 致矿侵入体的识别标志——以新疆阿尔夏提矽卡岩型铁铜矿床为例[J]. 岩石学报, 2014, 30(11):3455-3466. |
[12] | 罗照华, 陈必河, 江秀敏, 等. 利用宽谱系岩墙群进行勘查靶区预测的初步尝试:以南阿拉套山为例[J]. 岩石学报, 2012, 28(7) :1949-1965. |
[13] | 罗照华, 卢欣祥, 王秉璋, 等. 造山后脉岩组合与内生成矿作用[J]. 地学前缘, 2008, 15(4): 1-12. |
[14] | 罗照华, 莫宣学, 卢欣祥, 等. 透岩浆流体成矿作用——理论分析与野外证据[J]. 地学前缘, 2007, 14(3): 165-183. |
[15] | CONDIE K C. Plate Tectonics and Crustal Evolution[M]. Butterworth: Heinemann, 1997:1-282. |
[16] |
PETFORD N, CRUDEN A R, MCCAFFREY K J W, et al. Granite magma formation, transport and emplacement in the Earth’s crust[J]. Nature, 2000, 408:669-673.
DOI URL |
[17] | 李德东, 罗照华, 周久龙, 等. 岩墙厚度对成矿作用的约束:以石湖金矿为例[J]. 地学前缘, 2011, 18(1):166-178. |
[18] | 罗照华, 魏阳, 辛后田, 等. 造山后脉岩组合的岩石成因——对岩石圈拆沉作用的约束[J]. 岩石学报, 2006, 22(6):1672-1684. |
[19] |
EL-SAYED M M. Geochemistry and petrogenesis of the post-orogenic bimodal dyke swarms in NW Sinai, Egypt:Constraints on the magmatic-tectonic processes during the Late Precambrian[J]. Chemie der Erde, 2006, 66:129-141.
DOI URL |
[20] |
FÉMÉNIAS O, MERCIER J C C, NKONO C, et al. Calcic amphibole growth and compositions in calc-alkaline magmas: Evidence from the Motru dyke swarm (Southern Carpathians, Romania)[J]. American Mineralogist, 2006, 91:73-81.
DOI URL |
[21] |
FÉMÉNIAS O, BERZA T, TATU M, et al. Nature and significance of a Cambro-Ordovician high-K, calcic-alkaline sub-volcanic suite: The late- to post-orogenic Motru dyke swarm (Southern Carpathians, Romania)[J]. International Journal of Earth Science, 2008, 97:479-496.
DOI URL |
[22] | 倪守斌, 满发胜, 陈江峰, 等. 新疆阿拉套山成矿作用: 区域背景、矿源和模式[J]. 地质科学, 2009, 44(1):128-136. |
[23] | 王宗秀, 李春麟, NIKOLAIZ P, 等. 西天山造山带构造单元划分及古生代洋陆转换过程[J]. 中国地质, 2017, 44 (4):623-641. |
[24] | 曾祥武, 赵军, 聂晓勇. 新疆温泉县别珍套山新元古代花岗岩LA-ICP-MS锆石U-Pb年龄、地球化学特征及其成因[J]. 地质通报, 2020, 39(2/3):177-193. |
[25] | 李孔森, 王博, 舒良树, 等. 北天山温泉群的地质特征、时代和构造意义[J]. 高校地质学报, 2013, 19(3):491-503. |
[26] | 王仕林, 王根厚, 杜瑾雪, 等. 北天山西部温泉岩群中石榴角闪岩的岩石学和变质作用P-T轨迹研究[J]. 岩石学报, 2018, 34(12):3658-3670. |
[27] | 胡霭琴, 王中刚, 涂光炽, 等. 新疆北部地质演化及成岩成矿规律[M]. 北京: 科学出版社, 1997. |
[28] | 陈义兵, 胡霭琴, 张国新, 等. 西天山前寒武纪天窗花岗片麻岩的锆石U-Pb年龄及Sr-Nd同位素特征[J]. 地球化学, 1999, 28(6):515-519. |
[29] | 赵军, 关力伟, 朱永胜, 等. 中华人民共和国区域地质调查报告新疆温泉县扎冷木特幅(L44E018011)、柯克他乌幅(L44E018012)、牧区医院幅(L44E019011)、牙马特幅(L44E019012) 1∶5万地质矿产综合调查(1∶50000)[R]. 乌鲁木齐: 武警黄金第八支队, 2018. |
[30] |
YUAN H L, GAO S, LIU X M, et al. Accurate U-Pb age and trace element determinations of zircon by laser ablation-inductively coupled plasma-mass spectrometry[J]. Geostandards and Geoanalytical Research, 2004, 28(3):353-370.
DOI URL |
[31] |
ANDERSON T. Correction of common lead Pb in U-Pb analyses that do not report 204Pb[J]. Chemical Geology, 2002, 192(1/2):59-79.
DOI URL |
[32] | LUDWING K R. Isoplot, A Geochronological Toolkit for Microsoft Excel 3.00[M]. Berkeley: Berkeley Geochronology Center Special Publication, 2003:1-57. |
[33] |
LI C F, LI X H, LI Q L, et al. Rapid and precise determination of Sr and Nd isotopic ratios in geological samples from the same fillament loading by thermal ionization mass spectrometry employing a single-step separation scheme[J]. Analytica Chimica Acta, 2012, 727: 54-60.
DOI URL |
[34] |
LI C F, CHU Z Y, GUO J H, et al. A rapid single column separation scheme for high-precision Sr-Nd-Pb isotopic analysis in geological samples using thermal ionization mass spectrometry[J]. Analytical Methods, 2015, 7: 4793-4802.
DOI URL |
[35] |
HOSKIN P W O, SCHALTEGGER U. The composition of zircon and igneous and metamorphic petrogenesis[J]. Reviews in Mineralogy Geochemistry, 2003, 53(1):27-62.
DOI URL |
[36] |
MEZGER K, KROGSTAD L J. Interpretation of discordant U-Pb zircon ages: an evaluation[J]. Journal of Metamorphic Petrology, 1997, 15: 127-140.
DOI URL |
[37] | 刘飞, 杨经绥, 李天福, 等. 新疆北天山沙湾地区晚石炭世火山岩地球化学特征及地质意义[J]. 中国地质, 2011, 38(4): 868-889. |
[38] | 朱志新, 王克卓, 徐达, 等. 依连哈比尔尕山石炭纪侵入岩锆石SHRIMP U-Pb测年及其地质意义[J]. 地质通报, 2006, 25(8):986-991. |
[39] | 杨光华, 张炜波, 郭永峰, 等. 北天山四棵树花岗岩体锆石U-Pb年代学及地质意义[J]. 西北地质, 2014, 47(2): 83-98. |
[40] | 周泰禧, 陈江峰, 李学明. 新疆阿拉套山花岗岩类高εNd值的成因探讨[J]. 地质科学, 1996, 31(1):71-79. |
[41] | 胡霭琴, 韦刚健, 张积斌, 等. 西天山温泉地区早古生代斜长角闪岩的锆石SHRIMP U-Pb年龄及其地质意义[J]. 岩石学报, 2008, 24(12): 2731-2740. |
[42] | 王银喜, 李惠民, 陶仙聪, 等. 中天山东段花岗岩类钕锶氧同位素及地壳形成年龄[J]. 岩石学报, 1991, 24(3): 19-26. |
[43] | 韩宝福, 何国琦, 王式洗. 后碰撞慢源岩浆活动、底垫作用及准噶尔盆地基底的性质[J]. 中国科学(D辑), 1999, 29(1):16-21. |
[44] | 樊婷婷, 柳益群艺, 白清华, 等. 花岗岩类特征对准噶尔盆地基底性质的示踪[J]. 西安科技大学学报, 2017, 3(5):680-687. |
[45] | 吴福元, 江博明, 林强. 中国北方造山带造山后花岗岩的同位素特点与地壳生长意义[J]. 科学通报, 1997, 42(20):2188-2192. |
[46] |
WU F Y, SUN D Y, LI H M, et al. A-type granites in northeastern China: Age and geochemical constraints on their petrogenesis[J]. Chemical Geology, 2002, 187:143-173.
DOI URL |
[47] |
JAHN B M, WU F Y, CHEN B. Massive granitoid generation in central asia: Nd isotope evidence and implication for continental growth in the Phanerozoic[J]. Episodes, 2000, 23:82-92.
DOI URL |
[48] |
ZINDLER A, HART S. Chemical geodynamics[J]. Annual Review of Earth and Planetary Science, 1986, 14:493-571.
DOI URL |
[49] | HUGH R R. Using Geochemical Data:Evaluation, Presentation,Interpretation[M]. London, New York: Taylor and Francis Group, 1994:236-237. |
[50] | 徐学义, 夏林圻, 马中平, 等. 北天山巴音沟蛇绿岩斜长花岗岩SHRIMP锆石U-Pb年龄及蛇绿岩成因研究[J]. 岩石学报, 2006, 22(1):83-94. |
[51] |
ZHAO Z H, XIONG X L, WANG Q, et al. Underplating-related adakites in Xinjiang Tianshan, China[J]. Lithos, 2008, 102:374-391.
DOI URL |
[52] | 童英, 王涛, 洪大卫, 等. 北疆及邻区石炭—二叠纪花岗岩时空分布特征及其构造意义[J]. 岩石矿物学杂志, 2010, 29(6):619-641. |
[53] | 韩宝福, 郭召杰, 何国琦. “钉合岩体”与新疆北部主要缝合带的形成时限[J]. 岩石学报, 2010, 26(8):2233-2246. |
[54] | 徐学义, 马中平, 夏林圻, 等. 北天山巴音沟蛇绿岩形成时代的精确厘定及意义[J]. 地球科学与环境学报, 2005, 27(2):17-20. |
[55] |
HAN B F, GUO Z J, ZHANG Z C, et al. Age, geochemistry, and tectonic implications of a late Paleozoic stitching pluton in the North Tian Shan suture zone, western China[J]. Geological Society of America Bulletin, 2010, 122:627-640.
DOI URL |
[56] |
KIEMDR, JOHN T, SCHERER E E, et al. Changes in dip of subducted slabs at depth: Petrological and geochronological evidence from HP-UHP rocks (Tianshan, NW-China)[J]. Earth and Planetary Science Letters, 2011, 310(1/2):9-20.
DOI URL |
[57] | 朱志新, 董连慧, 王克卓, 等. 西天山造山带构造单元划分与构造演化[J]. 地质通报, 2013, 32(2) :297-306. |
[58] | 陈有炘, 裴先治, 赵军, 等. 西天山温泉地区下石炭统阿克沙克组碎屑锆石U-Pb年龄及其构造意义[J]. 地球科学, 2019, 35(7):2478-2492. |
[59] | 周晶, 季建清, 韩宝福, 等. 新疆北部基性岩脉 40Ar/39Ar年代学研究[J]. 地球科学, 2008, 24(5):997-1010. |
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FEATURES OF FRACTURED RESERVOIRS AND DEVELOPMENT LAW IN THE BASEMENT ROCK POOL IN DAMINTUN DEPRESSION, LIAOHE BASIN [J]. Geoscience, 2005, 19(Suppl): 273-277. |
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