Deformation Analyses and Their Geological Implications of Carboniferous-Permian Tectonic Transformation Period in Northwest Margin of Junggar Basin
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摘要: 通过对扎伊尔山至哈拉阿拉特山一带详细的构造变形分析, 揭示出准噶尔西北缘主要发育以下3组构造组合: 近南北向、北东-南西向和近东西向.其变形序列为: 晚石炭世早期, 发育近南北向褶皱-冲断构造; 晚石炭世时期, 近南北向构造线受牵引拖拽呈北东-南西向, 达尔布特、克拉玛依蛇绿混杂岩以右旋走滑拉出或侧向楔冲形式构造就位于上覆石炭系中; 晚石炭世晚期至二叠纪, 发育以达尔布特断裂为代表的北东-南西向伸展断裂, 伴随广泛的中基性岩脉及花岗岩侵入; 二叠纪末至三叠纪初, 发育广泛的近东西向劈理、哈山一带逆冲推覆构造及达尔布特左旋走滑活动.石炭纪至二叠纪, 西准地区经历了从俯冲到碰撞再到碰撞后陆内变形的演化过程, 伴随着挤压和伸展多期构造叠加, 充分体现了该地区复杂构造转换变形的动力学过程.Abstract: Detailed deformation analyses of the Zaire-Hala'alate Mountains show the following three different directional trends of regional structural features developed in the northwest margin of the Junggar basin: the south-north (S-N), northeast to southwest (NE-SW) and east-west (E-W) directions. The deformation sequences demonstrate that nearly S-N fold-thrust structures were developed during the early Late Carboniferous. During the late Late Carboniferous, nearly S-N tectonic orientation was transformed into the NE-SW direction by dragging. Meanwhile, the Darbut and Karamay ophiolitic mélanges were emplaced into the overlying Carboniferous strata by pulling-out under the control of dextral strike slip shearing or lateral wedge extrusion. Subsequently, NE-SW extensional faults, represented by the Darbut fault, were developed during the late Late Carboniferous to Permian, accompanied by extensive intrusion of intermediate to mafic dykes and granites. Between the end Permian and the Early Triassic, widespread E-W cleavages and thrust nappes in the Hala'alate Mountains were developed, and the Darbut sinistral strike slip fault was activated. From the Carboniferous to the Permian, the western Junggar underwent complicated evolutional processes including subduction, collision and intra-continental deformation, with multiphase tectonic overprints of compression and extension. The tectonic evolution history in the study area fully exhibits the regional geodynamic processes in the tectonic transformation deformation.
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图 1 中亚造山带构造分区
a.据Yang et al.(2012)改绘；b.研究区地质简图及剖面位置；c.白碱滩地质简图及闪长岩脉样品位置(N1016-1，GPS: 85°11′52.50″N, 45°51′52.65″E).1.第四系；2.新近系及古近系；3.下白垩统吐谷鲁群；4.上侏罗统齐古组；5.中侏罗统西山窑组；6.下侏罗统三工河组；7.下侏罗统八道湾组；8.上三叠统小泉沟组；9.上石炭-下二叠统佳木河组；10.中-上二叠统库吉尔台组；11.下-上石炭统哈拉阿拉特山组；12.下石炭统太勒古拉；13.下石炭统包古图组；14.下石炭统希贝库拉斯组；15.中泥盆统巴尔雷克组；16.中泥盆统库鲁木迪组；17.碱长花岗岩；18.花岗闪长岩；19.二长花岗岩；20.闪长岩脉(中基性岩墙)；21.蛇绿混杂岩
Fig. 1. Simplified tectonic divisions of the Central Asian orogenic belt
图 2 柳树沟-克拉玛依走廊带构造解剖及剖面
图a位置见图 1b
Fig. 2. Detailed structural maps and cross sections of the corridor from Liushugou to Karamay
图 3 成吉思汗山构造剖面(位置见图 1b，BJT-1)
1.凝灰质砂岩；2.凝灰质硅质粉砂岩；3.硅质岩；4.蛇纹片岩；5.玄武岩；6.硅质泥岩；7.凝灰质泥质砂岩；8.泥质砂岩；9.含砾砂岩；10.砂岩；11.砾岩；12.第四系；13.角度不整合界线；14.断层
Fig. 3. Structural cross section sketch of the Genghiskhan mountains
图 4 成吉思汗山构造变形特征
a、b.白碱滩一带褶皱及轴面产状；c.白碱滩褶皱轴面下半球极射赤平投影；d.白碱滩褶皱枢纽产状下半球极射赤平投影；e.晚期的正断层滑脱面及擦痕；f、g.白碱滩中基性岩脉展布特征；h.白碱滩中基性岩脉产状极点图
Fig. 4. Structural deformation characteristics of the Genghiskhan mountains
图 5 白碱滩地区克拉玛依蛇绿混杂岩构造变形特征
a.北亚带北西边界硅质岩透镜体；b.北亚带内部硅质岩透镜体；c.北亚带南东边界硅质岩透镜体及地层牵引；d.南亚带北西边界糜棱岩化及“σ型”透镜体；e、f.南亚带南东边界S型劈理化及玄武岩透镜体；g.玄武质透镜体受晚期左旋拉拽变形；h.佳木河组与蛇绿混杂岩呈角度不整合接触关系；i.佳木河组砾岩露头
Fig. 5. Structural deformation characteristics of the Karamay ophiolitic mélange in Baijiantan district
图 6 莫湖台地质构造剖面MHT-1
剖面MHT-1位置见图 1b.1.凝灰质砂岩；2.凝灰质硅质粉砂岩；3.硅质岩；4.蛇纹片岩；5.玄武岩；6.硅质泥岩；7.凝灰质泥质砂岩；8.泥质砂岩；9.含砾砂岩；10.断层；11.第四系
Fig. 6. Structural cross section MHT-1 sketch of Mohutai
图 7 达尔布特蛇绿混杂岩构造特征
a.玄武岩“S形”片理弯曲；b.蛇纹岩的“S形”强片理；c.玄武安山岩不对称透镜体呈右旋变形；d.紫红色硅质岩“σ型”构造透镜体；e.滑动面上的擦痕和阶步；f.构造透镜体被晚期左旋错断
Fig. 7. Structural deformation characteristics of the Darbut ophiolitic mélange
图 8 达尔布特断裂构造特征
a.达尔布特断层崖宏观；b.闪长岩脉被达尔布特次级断裂左旋切错(洛门沟)；c.残留蛇绿岩块体发生左旋肢解(石棉矿)；d.切错蛇纹岩，导致S形片理弯曲，指示剖面上的逆冲分量(达尔布特)；e.晚期正断层活动错落的闪长岩脉(达尔布特)
Fig. 8. Structural deformation characteristics of the Darbut fault
图 9 近南北向挤压作用形成的系列构造现象
a.近东西向劈理对近南北向延伸的硅质泥岩层的置换；b.劈理与近南北向层理的直交关系；c.东西向扩展形成的扩张石英脉
Fig. 9. Deformational structures formed by nearly NS compression
图 10 西准噶尔南部石炭系层理和劈理关系
位置见图 1b；黑色产状代表为层理；红色产状代表劈理
Fig. 10. Attitude relationship between bedding and cleavage in the Carboniferous strata of southern West Junggar
图 11 西准噶尔晚古生代花岗岩年龄统计直方图(a)和西准噶尔晚古生代中基性岩脉年龄统计直方图(b)
据a.高睿(2013)改绘
Fig. 11. Age histogram of the Late Paleozoic granitoids in the West Junggar (a) and Age histogram of the Late Paleozoic mafic dikes in the West Junggar (b)
表 1 西准噶尔中基性岩脉年龄及相关信息
Table 1. The geochronological information of intermediate to mafic dykes in the West Junggar
数据来源 方法 走向(°) 岩性 年龄(Ma) 样品位置 周晶等(2008) ICP-MS U-Pb 220 辉长岩 301.6 白碱滩后山 ICP-MS U-Pb 220 辉绿岩 313.9 白碱滩后山 李辛子等(2004) K-Ar 280~300 闪长玢岩 292.5±8.8 克拉玛依岩墙群 K-Ar 280~300 辉绿岩 265.5±5.4 克拉玛依岩墙群 K-Ar 280~300 闪长玢岩 271.5±8.1 克拉玛依岩墙群 K-Ar 280~300 辉长岩 267.1±8.0 克拉玛依岩墙群 康磊等(2009) ICP-MS U-Pb 280~310 辉绿岩、少量闪长质 296.9±9.8 夏尔莆岩体岩墙群 冯乾文等(2012a) ICP-MS U-Pb 310 闪长玢岩 303.1±1.2 克拉玛依岩墙群 角闪石Ar-Ar 310 闪长玢岩 312.1±2.8 克拉玛依岩墙群 徐芹芹(2008) 全岩Ar-Ar 220~230 辉绿岩 271.5±8.1 克拉玛依-达尔布特沿线 全岩Ar-Ar 220~230 闪长岩 265.6±5.4 全岩Ar-Ar 220~230 辉长岩 267.1±8.0 全岩Ar-Ar 220~230 辉绿岩 270.2±8.1 全岩Ar-Ar 220~230 闪长玢岩 256.5±7.7 Zhang et al.(2011) 全岩Ar-Ar 210~230 闪长岩 306.6±2.1 白碱滩野鸭沟 冯乾文等(2012b) ICP-MS U-Pb 环状100 闪长岩 304.0±1.0 红山岩体岩墙群 ICP-MS U-Pb 环状157 闪长岩 302.0±1.0 红山岩体岩墙群 ICP-MS U-Pb 环状78 闪长岩 303.0±1.0 红山岩体岩墙群 ICP-MS U-Pb 61 闪长玢岩 302.0±1.0 红山岩体岩墙群 ICP-MS U-Pb 94 闪长玢岩 302.0±1.0 红山岩体岩墙群 本项目 ICP-MS U-Pb 200~220 闪长岩 317.1±5.7 白碱滩后山 
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表 2 西准噶尔石炭-二叠纪构造转换期变形序列
Table 2. The deformation sequence of Carboniferous-Permian tectonic transformation period in West Junggar
序列 主要变形事件 发育时代 构造环境 伴生岩浆活动 D4 近南北向挤压，产生区带性、方位稳定的近东西向劈理，对早期褶皱-断裂构造产生横跨叠加；挤压分量产生系列北东向左旋走滑断裂，代表性的即达尔布特断裂和哈图北东向断裂系，切错其他不同方向构造，或牵引拖曳其他方向面理构造使之平行断裂的北东走向. 二叠纪末-三叠纪初 陆内挤压造山再次活动 陆内挤压-伸展交替 D3 达尔布特断裂正断层活动加剧，以库吉尔台组为代表的达尔布特河流相沉积开始发育；广泛的中基性岩墙群及碱性花岗岩侵入，以佳木河组为代表的陆内河流沉积形成. 晚石炭世晚期-二叠纪 后造山伸展 伸展型花岗岩及中基性岩脉 D2 近南北向褶皱-冲断构造被拖拽成北东-南西向，代表性的为成吉思汗山北东-南西向褶皱-断裂构造；达尔布特、白碱滩等蛇绿混杂岩系的右旋走滑或向南西方向的侧向楔冲变形，大陆边缘增生系统以右旋走滑拉出或侧向楔冲形式构造就位于上覆石炭系中. 晚石炭世 碰撞或后碰撞持续挤压 D1 柳树沟一带系列近南北向褶皱-冲断构造 晚石炭世早期 古亚洲洋闭合 岛弧型花岗岩
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Chen, B., Arakawa, Y., 2005. Elemental and Nd-Sr Isotopic Geochemistry of Granitoids from the West Junggar Foldbelt (NW China), with Implications for Phanerozoic Continental Growth. Geochimica et Cosmochimica Acta, 69(5): 1307-1320. doi: 10.1016/j.gca.2004.09.019 Chen, B., Jahn, B.M., 2004. Genesis of Post Collisional Granitoids and Basement Nature of the Junggar Terrane, NW China: Nd-Sr Isotope and Trace Element Evidence. Journal of Asian Earth Sciences, 23(5): 691-703. doi: 10.1016/S1367-9120(03)00118-4 Chen, B., Zhu, Y.F., 2011. Petrology, Geochemistry and Zircon U-Pb Chronology of Gabbro in Darbut Ophiolitic Mélange, Xinjiang. Acta Petrologica Sinica, 27(6): 1746-1758 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201106014.htm Chen, J.F., Han, B.F., Ji, J.Q., et al., 2010. Zircon U-Pb Ages and Tectonic Implications of Paleozoic Plutons in Northern West Junggar, North Xinjiang, China. Lithos, 115(1-4): 137-152. doi: 10.1016/j.lithos.2009.11.014 Chen, S., Guo, Z.J., 2010. Time Constraints, Tectonic Setting of Dalabute Ophiolitic Complex and Its Significance for Late Paleozoic Tectonic Evolution in West Junggar. Acta Petrologica Sinica, 26(8): 2336-2344 (in Chinese with English abstract). http://www.researchgate.net/publication/281549166_Time_constraints_tectonic_setting_of_Dalabute_ophiolitic_complex_and_its_significance_for_Late_Paleozoic_tectonic_evolution_in_West_Junggar Choulet, F., Faure, M., Cluzel, D., et al., 2012. From Oblique Accretion to Transpression in the Evolution of the Altaid Collage: New Insights from West Junggar, Northwestern China. Gondwana Research, 21(2-3): 530-547. doi: 10.1016/j.gr.2011.07.015 Feng, Q.W., Li, J.Y., Liu, J.F., et al., 2012a. Ages and Geological Significance of the Dark Dykes Emplaced in the Karamay Pluton and Adjacent Area, in Western Junggar, Xinjiang, NW China: Evidence from LA-ICP-MS Zircon Chronology and Ar-Ar Amphibole Chronology. Acta Petrologica Sinica, 28(7): 2158-2170 (in Chinese with English abstract). Feng, Q.W., Li, J.Y., Liu, J.F. et al., 2012b. Ages of the Hongshan Granite and Intruding Dioritic Dyke Swarms, in Western Junggar, Xinjiang, NW China: Evidence from LA-ICP-MS Zircon Chronology. Acta Petrologica Sinica, 28(9): 2935-2949 (in Chinese with English abstract). Gao, R., Xiao, L., Wang, G.C., et al., 2013. Paleozoic Magmatism and Tectonic Setting in West Junggar. Acta Petrologica Sinica, 29(10): 3413-3434 (in Chinese with English abstract). http://www.researchgate.net/publication/285747232_Paleozoic_Magmatism_and_Tectonic_Setting_in_West_Junggar Gu, P.Y., Li, Y.J., Zhang, B., et al., 2009. LA-ICP-MS Zircon U-Pb Dating of Gabbro in the Darbut Ophiolite, Western Junggar, China. Acta Petrologica Sinica, 25(6): 1364-1372 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200906008.htm Guan, S.W., Li, B.L., Hou, L.H., et al., 2008. New Hydrocarbon Exploration Areas in Footwall Covered Structures in Northwestern Margin of Junggar Basin. Petroleum Exploration and Development, 35(1): 17-22 (in Chinese with English abstract). doi: 10.1016/S1876-3804(08)60004-X Han, B.F., He, G.Q., Wang, S.G., et al., 1998. Postcollisional Mantle-Derived Magmatism and Vertical Growth of the Continental Crust in North Xinjiang. Geological Review, 44(4): 396-406 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP199804008.htm Han, B.F., Ji, J.Q., Song, B., et al., 2006. Late Paleozoic Vertical Growth of Continental Crust around the Junggar Basin, Xinjiang, China (Part I): Timing of Post-Collisional Plutonism. Acta Petrologica Sinica, 22(5): 1077-1086 (in Chinese with English abstract). http://www.researchgate.net/publication/269710583_Late_Paleozoic_vertical_growth_of_continental_crust_around_the_Junggar_Basin_Xinjiang_China_Part_I_Timing_of_post-collisional_plutonism Han, B.F., Wang, S.G., Jiang, B.M., et al., 1997. Nd Isotope Characteristics of the Wulungu River Alkali Granite in Xinjiang, China and Its Implication for Phanerozoic Continental Crust Growth. Chinese Science Bulletin, 42(17): 1829-1831 (in Chinese). doi: 10.1360/csb1997-42-17-1829 He, G.Q., Li, M.S., 1993. Some Problems of Ophiolite Geology in Northern China. Geological Research, 26: 3-12 (in Chinese with English abstract). He, G.Q., Liu, J.B., Zhang, Y.Q., et al., 2007. Keramay Ophiolitic Mélange Formed during Early Paleozoic in Western Junggar Basin. Acta Petrologica Sinica, 23(7): 1573-1576 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200707001.htm Kang, L., Li, Y.J., Zhang, B., et al., 2009. Petrographic Evidence for Magma Mixing of Xiaerpu Granite in West Junggar, Xinjiang. Acta Petrologica et Mineralogica, 28(5): 423-432 (in Chinese with English abstract). http://www.researchgate.net/publication/281606218_Petrographic_evidence_for_magma_mixing_of_Xiaerpu_granite_in_West_Junggar_Xinjiang Li, J.Y., He, G.Q., Xu, X., et al., 2006. Crustal Tectonic Framework of Northern Xinjiang and Adjacent Regions and Its Formation. Acta Geologica Sinica, 80(1): 148-168 (in Chinese with English abstract). http://www.researchgate.net/publication/286884899_Crustal_tectonic_framework_of_northern_Xinjiang_and_adjacent_regions_and_its_formation Li, W., 2007. The Mechanic and Tectonic Evolution of Mesozoic Basins in Northwestern Junggar Orogenic Belt (Dissertation). Chinese Academy of Geological Sciences, Beijing (in Chinese with English abstract). Li, X.Z., Han, B.F., Ji, J.Q., et al., 2004. Geology, Geochemistry and K-Ar Ages of the Karamay Basic-Intermediate Dyke Swarm from Xinjiang, China. Geochimica, 33(6): 574-584 (in Chinese with English abstract). http://www.researchgate.net/publication/313174990_Geology_geochemistry_and_K-Ar_ages_of_the_Karamay_basic-intermediate_dyke_swarm_from_Xinjiang_China Li, X.Z., Han, B.F., Li, Z.H., et al., 2005. Mechanism of the Karamay Basic-Intermediate Dyke Swarm from Xinjiang and Tectonic Implications. Geological Review, 51(5): 517-522 (in Chinese with English abstract). http://www.researchgate.net/publication/293144157_Mechanism_of_the_Karamay_basic-intermediate_dyke_swarm_from_Xinjiang_and_tectonic_implications Meng, J.F., Guo, Z.J., Fang, S.H., 2009. A New Insight into the Thrust Structures at the Northwestern Margin of Junggar Basin. Earth Science Frontiers, 16(3): 171-180 (in Chinese with English abstract). http://www.cqvip.com/QK/98600X/20093/30731173.html Shao, Y., Wang, R.F., Zhang, Y.Q., et al., 2011. Strike-Slip Structures and Oil-Gas Exploration in the NW Margin of the Junggar Basin, China. Acta Petrolei Sinica, 32(6): 976-984 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYXB201106008.htm Shu, L.S., Lu, H.F., Yin, D.H., et al., 2001. Late Paleozoic Continental Accretionary Tectonics in Northern Xinjiang. Xinjiang Geology, 19(1): 59-63 (in Chinese with English abstract). http://www.researchgate.net/publication/285732348_Late_Paleozoic_continental_accretionary_tectonics_in_northern_Xinjiang Su, Y.P., Tang, H.F., Hou, G.S., et al., 2006. Geochemistry of Aluminous A-Type Granites along Darabut Tectonic Belt in West Junggar, Xinjiang. Geochimica, 35(1): 55-67 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQHX200601006.htm Tong, Y., Wang, T., Hong, D.W., et al., 2010. Spatial and Temporal Distribution of the Carboniferous-Permian Granitoids in Northern Xinjiang and Its Adjacent Areas, and Its Tectonic Significance. Acta Petrologica et Mineralogica, 29(6): 619-641 (in Chinese with English abstract). http://www.cqvip.com/Main/Detail.aspx?id=35849233 Wang, R.F., 2012. Structural Analysis of Kelamay-Xiazijie Strike-Slip Fault Systems in NW Margin of Junggar Basin, Xinjiang, China (Dissertation). Zhejiang University, Hangzhou (in Chinese with English abstract). Wang, Y.J., Jin, Y.G., Jiang, N.Y., 1987. On the Age and Paleoenvironmental Features of the Hala alate Formation. Journal of Stratigraphy, 11(1): 53-57 (in Chinese with English abstract). http://www.researchgate.net/publication/287182828_On_the_Age_and_Paleoenvironmental_Features_of_the_Hala'alate_Formation Xiao, F.F., Hou, G.T., Wang, Y.X., et al., 2010. Study on Structural Stress Fields Since Permian, Junggar Basin and Adjacent Areas. Acta Scientiarum Naturalium Universitatis Pekinensis, 46(2): 224-230 (in Chinese with English abstract). http://www.researchgate.net/publication/290013835_Study_on_structural_stress_fields_since_Permian_Junggar_Basin_and_adjacent_areas Xiao, W.J., Han, C.M., Yuan, C., et al., 2006. Unique Carboniferous-Permian Tectonic-Metallogenic Framework of Northern Xinjiang (NW China): Constraints for the Tectonics of the Southern Paleoasian Domain. Acta Petrologica Sinica, 22(5): 1062-1076 (in Chinese with English abstract). http://ci.nii.ac.jp/naid/10026539172 Xiao, W.J., Han, C.M., Yuan, C., et al., 2008. Middle Cambrian to Permian Subduction-Related Accretionary Orogenesis of Northern Xinjiang, NW China: Implications for the Tectonic Evolution of Central Asia. Journal of Asian Earth Sciences, 32(2-4): 102-117. doi: 10.1016/j.jseaes.2007.10.008 Xiao, X.C., Tang, Y.Q., Feng, Y.M., et al., 1992. Tectonic Evolution of the Northern Xinjiang and Its Adjacent Regions. Geological Publishing House, Beijing (in Chinese with English abstract). Xu, Q.Q., Ji, J.Q., Han, B.F., et al., 2008. Petrology, Geochemistry and Geochronology of the Intermediate to Mafic Dykes in Northern Xinjiang since Late Paleozoic. Acta Petrologica Sinica, 24(5): 977-996 (in Chinese with English abstract). http://www.oalib.com/paper/1473499 Xu, X., He, G.Q., Li, H.Q., et al., 2006. Basic Characteristics of the Karamay Ophiolitic Mélange, Xinjiang, and Its Zircon SHRIMP Dating. Geology in China, 33(3): 470-475 (in Chinese with English abstract). http://www.researchgate.net/publication/279580642_Basic_characteristics_of_the_Karamay_ophiolitic_mlange_Xinjiang_and_its_zircon_SHRIMP_dating Xu, X., Zhou, K.F., Wang, Y., 2010. Study on Extinction of the Remnant Oceanic Basin and Tectonic Setting of West Junggar During Late Paleozoic. Acta Petrologica Sinica, 26(11): 3206-3214 (in Chinese with English abstract). http://www.cqvip.com/QK/94579X/201011/1003851225.html Yang, G., Wang, X.B., Li, B.L., et al., 2009. Oblique Compressional Structures and Hydrocarbon Distribution Patterns in the Northwestern Margin of the Junggar Basin. Oil and Gas Geology, 30(1): 26-32 (in Chinese with English abstract). http://www.cqvip.com/qk/95357X/200901/29747557.html Yang, G.X., Li, Y.J., Gu, P.Y., et al., 2012. Geochronological and Geochemical Study of the Darbut Ophiolitic Complex in the West Junggar (NW China): Implications for Petrogenesis and Tectonic Evolution. Gondwana Research, 21(4): 1037-1049. doi: 10.1016/j.gr.2011.07.029 Yin, J.Y., Yuan, C., Sun, M., et al., 2009. Sanukitic Dykes in West Junggar, Xinjiang: Geochemical Features, Petrogenesis and Links to Cu-Au Mineralization. Geochimica, 38(5): 413-423 (in Chinese with English abstract). http://www.researchgate.net/publication/285649516_Sanukitic_dykes_in_West_Junggar_Xinjiang_Geochemical_features_petrogenesis_and_links_to_Cu-Au_mineralization You, Q.M., 1983. The Nappe Tectonic Research of the Northwestern Margin of the Junggar Basin. Xinjiang Petroleum Geology, 1: 6-16 (in Chinese). Zhang, C., Huang, X., 1992. The Ages and Tectonic Settings of Ophiolites in West Junggar, Xinjiang. Geological Review, 38(6): 509-524 (in Chinese with English abstract). http://www.researchgate.net/publication/312462444_Age_and_tectonic_settings_of_ophiolites_in_west_Junggar_Xinjiang Zhang, J.E., Xiao, W.J., Han, C.M., et al., 2009. Fold-and-Thrust Structure in Yeyagou Area, Western Junggar, China and Its Implication. Geological Bulletin of China, 28(12): 1894-1903 (in Chinese with English abstract). http://www.researchgate.net/publication/281245167_Fold-and-thrust_structure_in_Yeyagou_area_western_Junggar_China_and_its_implication Zhang, J.E., Xiao, W.J., Han, C.M., et al., 2011. Kinematics and Age Constraints of Deformation in a Late Carboniferous Accretionary Complex in Western Junggar, NW China. Gondwana Research, 19(4): 958-974. doi: 10.1016/j.gr.2010.10.003 Zhang, L., Wang, G.C., Gao, R., et al., 2015. U-Pb Chronology of Carboniferous Detrital Zircons and Its Geological Implications in West Junggar. Geotectonica et Metallogenia, in press (in Chinese with English abstract). Zhang, L.C., Wan, B., Jiao, X.J., et al., 2006. Characteristics and Geological Significance of Adakitic Rocks in Copper-Bearing Porphyry in Baogutu, Western Junggar. Geology in China, 33(3): 626-631 (in Chinese with English abstract). http://d.wanfangdata.com.cn/Periodical/zgdizhi200603020 Zhang, L.F., Xian, W.S., Sun, M., 2004. Petrogenesis of Charnockites from Western Junggar, Xinjiang, China. Xinjiang Geology, 22(1): 36-42 (in Chinese with English abstract). http://www.researchgate.net/publication/285727744_Petrogenesis_of_charnockites_from_western_Junggar_Xinjiang_China Zhang, Y.Q., Wang, X., Liu, J.S., et al., 2011. Wuerhe-Xiazijie Strike-Slip Structure and Petroleum Exploration Significance in Northwestern Margin of Junggar Basin. Xinjiang Petroleum Geology, 32(5): 447-450 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-XJSD201105003.htm Zhou, J., Ji, J.Q., Han, B.F., et al., 2008. 40Ar/39Ar Geochronology of Mafic Dykes in North Xinjiang. Acta Petrologica Sinica, 24(5): 997-1010 (in Chinese with English abstract). http://www.zhangqiaokeyan.com/academic-journal-cn_acta-petrologica-sinica_thesis/0201252027464.html Zhu, Y.F., Chen, B., Xu, X., et al., 2013. A New Geological Map of the Western Junggar, North Xinjiang (NW China): Implications for Paleoenvironmental Reconstruction. Episodes, 36(3): 205-220. doi: 10.18814/epiiugs/2013/v36i3/003 Zhu, Y.F., Xu, X., Wei, S.N., et al., 2007. Geochemistry and Tectonic Significance of OIB-Type Pillow Basalts in Western Mts. of Karamay City (Western Junggar), NW China. Acta Petrologica Sinica, 23(7): 1739-1748 (in Chinese with English abstract). http://www.oalib.com/paper/1471352 Zong, R.W., Gong, Y.M., Wang, G.C., 2014. Carboniferous Stratal Sequence and Its Palaeogeographical Evolution in Southern Western Junggar, NW China. Earth Science Frontiers, 21(2): 216-233 (in Chinese with English abstract). http://d.wanfangdata.com.cn/Periodical/dxqy201402016 陈博, 朱永峰, 2011. 新疆达拉布特蛇绿混杂岩中辉长岩岩石学、微量元素地球化学和锆石U-Pb年代学研究. 岩石学报, 27(6): 1746-1758. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201106014.htm 陈石, 郭召杰, 2010. 达拉布特蛇绿岩带的时限和属性以及对西准噶尔晚古生代构造演化的讨论. 岩石学报, 26(8): 2336-2344. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201008010.htm 冯乾文, 李锦轶, 刘建峰, 等, 2012a. 新疆西准噶尔克拉玛依岩体中暗色岩墙的形成时代及地质意义——来自锆石LA-ICP-MS和角闪石Ar-Ar定年的证据. 岩石学报, 28(7): 2158-2170. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201207018.htm 冯乾文, 李锦轶, 刘建峰, 等, 2012b. 新疆西准噶尔红山岩体及其中闪长质岩墙的时代——来自锆石LA-ICP-MS定年的证据. 岩石学报, 28(9): 2935-2949. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201209022.htm 高睿, 肖龙, 王国灿, 等, 2013. 西准噶尔晚古生代岩浆活动和构造背景. 岩石学报, 29(10): 3413-3434. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201310008.htm 辜平阳, 李永军, 张兵, 等, 2009. 西准达尔布特蛇绿岩中辉长岩LA-ICP-MS锆石U-Pb测年. 岩石学报, 25(6): 1364-1372. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200906008.htm 管树巍, 李本亮, 侯连华, 等, 2008. 准噶尔盆地西北缘下盘掩伏构造油气勘探新领域. 石油勘探与开发, 35(1): 17-22. doi: 10.3321/j.issn:1000-0747.2008.01.004 韩宝福, 何国琦, 王式洸, 等, 1998. 新疆北部后碰撞幔源岩浆活动与陆壳纵向生长. 地质评论, 44(4): 396-406. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP199804008.htm 韩宝福, 季建清, 宋彪, 等, 2006. 新疆准噶尔晚古生代陆壳垂向生长(Ⅰ)——后碰撞深成岩浆活动的时限. 岩石学报, 22(5): 1077-1086. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200605003.htm 韩宝福, 王式洸, 江博明, 等, 1997. 新疆乌伦古河碱性花岗岩Nd同位素特征及其对显生宙地壳生长的意义. 科学通报, 42(17): 1829-1831. doi: 10.3321/j.issn:0023-074X.1997.17.011 何国琦, 李茂松, 1993. 中国兴蒙-北疆蛇绿岩地质的若干问题. 地学研究, 26: 3-12. https://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGDJ199400002003.htm 何国琦, 刘建波, 张越迁, 等, 2007. 准噶尔盆地西缘克拉玛依早古生代蛇绿混杂岩带的厘定. 岩石学报, 23(7): 1573-1576. doi: 10.3969/j.issn.1000-0569.2007.07.002 康磊, 李永军, 张兵, 等, 2009. 新疆西准噶尔夏尔莆岩体岩浆混合的岩相学证据. 岩石矿物学杂志, 28(5): 423-432. doi: 10.3969/j.issn.1000-6524.2009.05.002 李锦轶, 何国琦, 徐新, 等, 2006. 新疆北部及邻区地壳构造格架及其形成过程的初步探讨. 地质学报, 80(1): 148-168. doi: 10.3321/j.issn:0001-5717.2006.01.017 李玮, 2007. 准噶尔西北缘造山带中生代盆地形成机制及构造演化(博士学位论文). 北京: 中国地质科学院. 李辛子, 韩宝福, 季建清, 等, 2004. 新疆克拉玛依中基性岩墙群的地质地球化学和K-Ar年代学. 地球化学, 33(6): 574-584. doi: 10.3321/j.issn:0379-1726.2004.06.005 李辛子, 韩宝福, 李宗怀, 等, 2005. 新疆克拉玛依中基性岩墙群形成力学机制及其构造意义. 地质评论, 51(5): 517-522. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP200505006.htm 孟家峰, 郭召杰, 方世虎, 2009. 准噶尔盆地西北缘冲断构造新解. 地学前缘, 16(3): 171-180. doi: 10.3321/j.issn:1005-2321.2009.03.013 邵雨, 汪仁富, 张越迁, 等, 2011. 准噶尔盆地西北缘走滑构造与油气勘探. 石油学报, 32(6): 976-984. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB201106008.htm 舒良树, 卢华复, 印栋浩, 等, 2001. 新疆北部古生代大陆增生构造. 新疆地质, 19(1): 59-63. doi: 10.3969/j.issn.1000-8845.2001.01.011 苏玉平, 唐红峰, 侯广顺, 等, 2006. 新疆西准噶尔达拉布特构造带铝质A型花岗岩的地球化学研究. 地球化学, 35(1): 55-67. https://www.cnki.com.cn/Article/CJFDTOTAL-DQHX200601006.htm 童英, 王涛, 洪大卫, 等, 2010. 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. 岩石矿物学杂志, 29(6): 619-641. doi: 10.3969/j.issn.1000-6524.2010.06.003 汪仁富, 2011. 准噶尔盆地西北缘克拉玛依-夏子街走滑构造(博士学位论文). 杭州: 浙江大学. 王玉净, 金玉玕, 江纳言, 1987. 论哈拉阿拉特组的时代及古环境特征. 地层学杂志, 11(1): 53-57. https://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ198701005.htm 肖芳峰, 侯贵廷, 王延欣, 等, 2010, 准噶尔盆地及周缘二叠纪以来构造应力场解析. 北京大学学报(自然科学版), 46(2): 224-230. https://www.cnki.com.cn/Article/CJFDTOTAL-BJDZ201002010.htm 肖文交, 韩春明, 袁超, 等, 2006. 新疆北部石炭纪-二叠纪独特的构造-成矿作用: 对古亚洲洋构造域南部大地构造演化的制约. 岩石学报, 22(5): 1062-1076. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200605002.htm 肖序常, 汤耀庆, 冯益民, 等, 1992. 新疆北部及其邻区大地构造. 北京: 地质出版社. 徐芹芹, 季建清, 韩宝福, 等, 2008. 新疆北部晚古生代以来中基性岩脉的年代学、岩石学、地球化学研究. 岩石学报, 24(5): 977-996. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200805006.htm 徐新, 何国琦, 李华芹, 等, 2006. 克拉玛依蛇绿混杂岩带的基本特征和锆石SHRIMP年龄信息. 中国地质, 33(3): 470-475. doi: 10.3969/j.issn.1000-3657.2006.03.003 徐新, 周可法, 王煜, 2010. 西准噶尔晚古生代残余洋盆消亡时间与构造背景研究. 岩石学报, 26(11): 3206-3214. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201011005.htm 杨庚, 王晓波, 李本亮, 等, 2009. 准噶尔盆地西北缘斜向挤压构造与油气分布规律. 石油与天然气地质, 30(1): 26-32. doi: 10.3321/j.issn:0253-9985.2009.01.004 尹继元, 袁超, 孙敏, 等, 2009. 新疆西准噶尔地区赞岐岩(sanukite)的地球化学特征、成因机制及其与铜金矿化的关系. 地球化学, 38(5): 413-423. doi: 10.3321/j.issn:0379-1726.2009.05.001 尤绮妹, 1983. 准噶尔盆地西北缘推复构造的研究. 新疆石油地质, 1: 6-16. https://www.cnki.com.cn/Article/CJFDTOTAL-XJSD198301002.htm 张弛, 黄萱, 1992. 新疆西准噶尔蛇绿岩形成时代和环境的探讨. 地质论评, 38(6): 509-524. doi: 10.3321/j.issn:0371-5736.1992.06.009 张继恩, 肖文交, 韩春明, 等, 2009. 西准噶尔野鸭沟地区褶皱冲断构造的特征及意义. 地质通报, 28(12): 1894-1903. doi: 10.3969/j.issn.1671-2552.2009.12.021 张立飞, 冼伟胜, 孙敏, 2004. 西准噶尔紫苏花岗岩成因岩石学研究. 新疆地质, 22(1): 36-42. doi: 10.3969/j.issn.1000-8845.2004.01.007 张连昌, 万博, 焦学军, 等, 2006. 西准包古图含铜斑岩的埃达克岩特征及其地质意义. 中国地质, 33(3): 626-631. doi: 10.3969/j.issn.1000-3657.2006.03.020 张雷, 王国灿, 高睿, 等, 2015. 新疆西准噶尔石炭系碎屑锆石U-Pb年代学及其地质意义. 大地构造与成矿, 待刊. 张越迁, 汪新, 刘继山, 等, 2011. 准噶尔盆地西北缘乌夏走滑构造及油气勘探意义. 新疆石油地质, 32(5): 447-450. https://www.cnki.com.cn/Article/CJFDTOTAL-XJSD201105003.htm 周晶, 季建清, 韩宝福, 等, 2008. 新疆北部基性岩脉40Ar/39Ar年代学研究. 岩石学报, 24(5): 997-1010. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200805007.htm 朱永峰, 徐新, 魏少妮, 等, 2007. 西准噶尔克拉玛依OIB型枕状玄武岩地球化学及其地质意义研究. 岩石学报, 23(7): 1739-1748. doi: 10.3969/j.issn.1000-0569.2007.07.019 纵瑞文, 龚一鸣, 王国灿, 2014. 西准噶尔南部石炭纪地层层序及古地理演化. 地学前缘, 21(2): 216-233. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201402018.htm -
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