[1] Deng, S.H., Du, P.D., Lu, Y.Z., et al., 2015.Unconformities in the Ordovician of Tazhong-Bachu Area of the Tarim Basin, NW China.Geological Review, 61(2):324-332(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DZLP201502009.htm
[2] Du, P.D., Yang, Z.L., Zhao, Z.X., et al., 2013.Discussion on the Age of the Ordovician Yiangshan Formation in Tarim Block.Journal of Stratigraphy, 37(2):223-231(in Chinese with English abstract).
[3] Fang, D.J., Shen, Z.Y., Wang, P.Y., 2001.Paleomagnetic Data of Tarim Block.Journal of Zhejiang University(Science Edition), 28(1):92-99 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HZDX200101016.htm
[4] Feng, Z.Z., Bao, Z.D., Wu, M.B., et al., 2007.Lithofacies Palaeogeography of the Ordovician in Tarim Area.Journal of Palaeogeography, 9(5):447-460(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GDLX200705005.htm
[5] Gao, X.F., Xiao, P.X., Kang, L., et al., 2013.Origin of Datongxi Pluton in the West Kunlun Orogen:Constraints from Mineralogy, Elemental Geochemistry and Zircon U-Pb Age.Acta Petrologica Sinica, 29(9):3065-3079(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201309009.htm
[6] Gao, Z.Q., Fan, T.L., Yang, W.H., et al., 2012.Structure Characteristics and Evolution of the Eopaleozoic Carbonate Platform in Tarim Basin.Journal of Jilin University, 42(3):657-665(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CCDZ201203009.htm
[7] Ge, R.F., Zhu, W.B., Wu, H.L., et al., 2012.The Paleozoic Northern Margin of the Tarim Craton:Passive or Active.Lithos, 142-143:1-15. https://doi.org/10.1016/j.lithos.2012.02.010
[8] Han, J.F., Sun, C.H., Wang, Z.Y., et al., 2017.Superimposed Compound Karst Model and Oil and Gas Exploration of Carbonate in Tazhong Uplift.Earth Science, 42(3):410-420. https://doi.org/10.3799/dqkx.2017.031
[9] He, D.F., Jia, C.Z., Li, D.S., et al., 2005.Formation and Evolution of Polycyclic Superimposed Tarim Basin.Oil & Gas Geology, 26(1):64-77(in Chinese with English abstract). http://en.cnki.com.cn/article_en/cjfdtotal-syyt200501009.htm
[10] He, D.F., Zhou, X.Y., Zhang, C.J., et al., 2007.The Evolution of Prototype Basins During Ordovician in Tarim Area.Chinese Science Bulletin, 52(S1):126-135(in Chinese).
[11] Huang, B.C., Zhou, Y.X., Zhu, R.X., 2008.Discussions on Phanerozoic Evolution and Formation of Continental China.Earth Science Frontiers, 15(3):348-359(in Chinese with English abstract). http://en.cnki.com.cn/article_en/cjfdtotal-dxqy200803034.htm
[12] Jia, C.Z., 1997.Tectonic Characteristics and Petroleum of the Tarim Basin, China.Petroleum Industry Press, Beijing(in Chinese).
[13] Jiang, T., Gao, J., Reiner, K., et al., 2014.Paleozoic Ophiolitic Mélanges from the South Tianshan Orogen, NW China:Geological, Geochemical and Geochronological Implications for the Geodynamic Setting.Tectonophysics, 612-613:106-127. https://doi.org/10.1016/j.tecto.2013.11.038
[14] Kang, L., Liu, L., Cao, Y.T., et al., 2011.Geochemistry, Zircon LA-ICP-MS U-Pb Ages and Hf Isotopes of Hongliugou Moyite from North Altyn Tagh Tectonic Belt.Geological Bulletin of China, 30(7):1066-1076(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD201107008.htm
[15] Li, J.H., Wang, H.H., Li, W.B., et al., 2014.Discussion on Global Tectonics Evolution from Plate Reconstruction in Phanerozoic.Acta Petrolei Sinica, 35(2):207-218(in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTotal-SYXB201402001.htm
[16] Li, P.J., Chen, H.H., Tang, D.Q., et al., 2017.Coupling Relationship between NE Strike-Slip Faults and Hypogenic Karstification in Middle-Lower Ordovician of Shunnan Area, Tarim Basin, Northwest China.Earth Science, 42(1):93-104. https://doi.org/10.3799/dqkx.2017.007
[17] Lin, C.S., Yang, H.J., Liu, J.Y., et al., 2012.Distribution and Erosion of the Paleozoic Tectonic Unconformities in the Tarim Basin, Northwest China:Significance for the Evolution of Paleo-Uplifts and Tectonic Geography During Deformation.Journal of Asian Earth Sciences, 46(11):1-19. https://doi.org/10.1016/j.jseaes.2011.10.004
[18] Liu, W., Zhang, X.Y., Gu, J.Y., et al., 2009.Sedimentary Environment of Lower Middle Ordovician Yingshan Formation in Mid-Western Tarim Basin.Acta Sedimentologica Sinica, 27(3):435-442(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CJXB200903007.htm
[19] Liu, Z.B., Gao, S.L., Liu, S.L., et al., 2015.Ordovician Carbonate Sedimentary Characteristics and Models of Bachu-Maigaiti Region in Tarim Basin.Journal of Central South University(Science and Technology), 46(11):4165-4173(in Chinese with English abstract).
[20] Qi, X.X., Li, H.B., Wu, C.L., et al.2005.SHRIMP Age of Qiashenkansayi Granodiorite and Its Geological Significance in North Altun.Chinese Science Bulletin, 50(6):571-576(in Chinese). doi: 10.1007/s11430-006-2041-6
[21] Shen, A.J., Zhao, W.Z., Hu, A.P., et al.2015.Major Factors Controlling the Development of Marine Carbonate Reservoirs.Petroleum Exploration and Development, 42(5):1-10(in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTOTAL-SKYK201505001.htm
[22] Shi, R.D., Yang, J.S., Wu, C.L., et al., 2004.First SHRIMP Dating for the Formation of the Late Sinian Yushugou ophiolite, North Qilian Mountains.Acta Geologica Sinica, 78(5):649-657(in Chinese with English abstract).
[23] Sun, C.H., Yu, H.F., Wang, H.S., et al., 2012.Vugular Formation of Carbonates in Ordovician Yingshan Reservoir in Tazhong Northern Slope of Tarim Basin.Natural Gas Geoscience, 23(2):230-236(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-TDKX201202006.htm
[24] Wang, B., Shu, L.S., Michel, F., et al., 2011.Paleozoic Tectonics of the Southern Chinese Tianshan:Insights from Structural, Chronological and Geochemical Studies of the Heiyingshan Ophiolitic Mélange (NW China).Tectonophysics, 497(11):85-104. https://doi.org/10.1016/j.tecto.2010.11.004
[25] Wang, C.L., Wu, G.H., Cui, W.J., et al., 2011.Characteristics and Distribution of Intra-Platform Beach of the Lower-Middle Ordovician Yingshan Formation Carbonate in Tarim Basin.Acta Sedimentologica Sinica, 29(6):1048-1057(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CJXB201106005.htm
[26] Wang, T.G., Song, D.F., Li, M.J., et al., 2014.Natural Gas Source and Deep Gas Exploration Potential of the Ordovician Yingshan Formation in the Shunnan-Gucheng Region, Tarim Basin.Oil & Gas Geology, 35(6):753-762(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-SYYT201406003.htm
[27] Wu, C.L., Yang, J.S., Yao, S.Z., et al., 2005.Characteristics of the Granitoid Complex and Its Zircon SHRIMP Dating at the South Margin of the Bashikaogong, North Altun, NW China.Acta Petrologica Sinica, 21(3):846-858(in Chinese with English abstract). http://www.oalib.com/paper/1473151
[28] Wu, C.L., Yao, S.Z., Zeng, L.S., et al., 2007.Petrology and SHRIMP Age of Granite at Bashikaogong-Simierbulake, North Altun.Science China Earth Science, 37(1):10-26(in Chinese). https://www.sciencedirect.com/science/article/pii/S0024493709002059
[29] Wu, X.N., Si, C.S., Yu G., et al., 2012.Reconstruction of Ordovician Lithofaceis Palaeogeography and Petroleum Prospecting Significance in Tarim Basin.Marine Petroleum Geology, 17(3):9-17(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HXYQ201203004.htm
[30] Xiao, W.J., Hou, Q.L., Li, J.L., et al., 2000.Tectonics Phases Anatomy and Process of Multi-Arcs Hyperplasia in West Kunlun.Science China Earth Science, 30(Suppl.):22-28(in Chinese).
[31] Xiao, X.C., Wang, J., Su, L., et al., 2003.A Further Discussion of the Kuda Ophiolite, West Kunlun, and Its Tectonic Significance.Geological Bulletin of China, 22(10):745-750(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD200310000.htm
[32] Xiong, J.F., Yu, T.X., Cao, Z.C., et al., 2013.The Breakup of the Ordovician Yingshan Formation and the Lower-Middle Ordovician Boundary in the Tarim Basin.Journal of Stratigraphy, 37(3):283-291(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DCXZ201303005.htm
[33] Xiu, Q.Y., Yu, H.F., Liu, Y.S., et al., 2007.Geology and Zircon U-Pb Age of Pillow Basalt at Qiashikansoy in Northern Altum Tagh.Acta Geologica Sinica, 81(6):787-794(in Chinese with English abstract). http://en.cnki.com.cn/article_en/cjfdtotal-dzxe200706005.htm
[34] Xu, X.S., Wang, Z.J., Wan, F., et al., 2005.Tectonic Paleogeographic Evolution and Source Rocks of the Early Paleozoic in the Tarim Basin.Earth Science Frontiers, 12(3):49-57(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DXQY200503007.htm
[35] Xu, X.Z., Yang, J.S., Guo, G.L., et al., 2011.The Yushugou-Tonghuashan Ophiolites in Tianshan, Xinjiang, and Their Tectonic Setting.Acta Petrologica Sinica, 27(1):96-120(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201101007.htm
[36] Xu, Z.Q., Li, S.T., Zhang, J.X., et al., 2011.Paleo-Asian and Tethyan Tectonic Systems with Docking the Tarim Block.Acta Petrologica Sinica, 27(1):1-22(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YSXB201101002.htm
[37] Yan, W., Wang, X.Z., Wang, Z.Y., et al., 2010.New Evidence on the Sedimentary Framework of the Early Ordovician in Central Tarim and Adjacent Area.Acta Sedimentologica Sinica, 28(6):1090-1097(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CJXB201006007.htm
[38] Yang, J.S., Shi, R.D., Wu, C.L., et al., 2008.Petrology and SHRIMP Age of the Hongliugou Ophiolite at Milan, North Altun, at the Northern Margin of the Tibetan Plateau.Acta Petrologica Sinica, 24(7):1567-1584(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YSXB200807014.htm
[39] Yang, J.S., Xu, X.Z., Li, T.F., et al., 2011.U-Pb Ages of Zircons from Ophiolite and Related Rocks in the Kumishi Region at the Southern Margin of Middle Tianshan, Xinjiang:Evidence of Early Paleozoic Oceanic Basin.Acta Petrologica Sinica, 27(1):77-95(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201101006.htm
[40] Ye, H.M., Li, X.H., Li, Z.X., et al., 2008.Age and Origin of High Ba-Sr Appinite-Granites at the Northwestern Margin of the Tibet Plateau:Implications for Early Paleozoic Tectonic Evolution of the Western Kunlun Orogenic Belt.Gondwana Research, 13:126-138. https://doi.org/10.1016/j.gr.2007.08.005
[41] Ying, D.G., Zheng, Y.Z., Gong, X.P., et al., 2013.The Geological Characteristics and Formation Epoch of West Kunlun Kudi Petrofabric.Xinjiang Geology, 31(4):281-286(in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTOTAL-XJDI201304003.htm
[42] Yu, B.S., Lin, C.S., Fan, T.L., et al., 2011.Sedimentary Response to Geodynamic Reversion in Tarim Basin during Cambrian and Ordovician and Its Significance to Reservoir Development.Earth Science Frontiers, 18(3):221-231(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY201103023.htm
[43] Yu, S.Y., Zhang, J.X., Pablo, G.R., et al., 2013.The Grenvillian Orogeny in the Altun-Qilian-North Qaidam Mountain Belts of Northern Tibet Plateau:Constraints from Geochemical and Zircon U-Pb Age and Hf Isotopic Study of Magmatic Rocks.Journal of Asian Earth Sciences, 73:372-395. https://doi.org/10.1016/j.jseaes.2013.04.042
[44] Zhang, C.L., Zou, H.B., Li, H.K., et al., 2013.Tectonic Framework and Evolution of the Tarim Block in NW China.Gondwana Research, 23:1306-1315. doi: 10.1016/j.gr.2012.05.009
[45] Zhang, J.X., Zhang, Z.M., Xu, Z.Q., et al., 2001.Petrology and Geochronology of Eclogites from the Western Segment of the Altyn Tagh, Northwestern China.Lithos, 56:187-206. doi: 10.1016/S0024-4937(00)00052-9
[46] Zhang, L.J., Li, Y., Zhou, C.G., et al., 2007.Lithofacies Paleogeographical Characteristics and Reef-Shoal Distribution during the Ordovician in the Tarim Basin.Oil & Gas Geology, 28(6):731-737(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYYT200706006.htm
[47] Zhao, W.Z., Shen, A.J., Pan, W.Q., et al., 2013.A Research on Carbonate Karst Reservoirs Classification and Its Implication on Hydrocarbon Exploration:Cases Studies From Tarim Basin.Acta Petrologica Sinica, 29(9):3213-3222(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201309020.htm
[48] Zhao, Z.J., Wu, X.N., Pan, W.Q., et al., 2009.Sequence Lithofacies Palaeogeography during the Ordovician in the Tarim Basin.Acta Sedimentologica Sinica, 27(5):939-955(in Chinese with English abstract). doi: 10.1007/s12517-016-2557-9
[49] 邓胜徽, 杜品德, 卢远征, 等, 2015.塔里木盆地塔中-巴楚地区奥陶系内幕不整合.地质论评, 61(2):324-332. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dzlp201502009&dbname=CJFD&dbcode=CJFQ
[50] 杜品德, 杨芝林, 赵治信, 等, 2013.塔里木板块奥陶系鹰山组的地质时代.地层学杂志, 37(2):223-231. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dcxz201302015&dbname=CJFD&dbcode=CJFQ
[51] 方大钧, 沈忠悦, 王朋岩, 2001.塔里木板块古地磁数据表.浙江大学学报(理学版), 28(1):92-99. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=hzdx200101016&dbname=CJFD&dbcode=CJFQ
[52] 冯增昭, 鲍志东, 吴茂炳, 等, 2007.塔里木地区奥陶纪岩相古地理.古地理学报, 9(5):447-460. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=gdlx200705005&dbname=CJFD&dbcode=CJFQ
[53] 高晓峰, 校培喜, 康磊, 等, 2013.西昆仑大同西岩体成因:矿物学、地球化学和锆石U-Pb年代学制约.岩石学报, 29(9):3065-3079. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb201309009&dbname=CJFD&dbcode=CJFQ
[54] 高志前, 樊太亮, 杨伟红, 等, 2012.塔里木盆地下古生界碳酸盐岩台缘结构特征及其演化.吉林大学学报, 42(3):657-665. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ccdz201203009&dbname=CJFD&dbcode=CJFQ
[55] 韩剑发, 孙崇浩, 王振宇, 等, 2017.塔中隆起碳酸盐岩叠合复合岩溶模式与油气勘探.地球科学, 42(3):410-420. https://doi.org/10.3799/dqkx.2017.031
[56] 何登发, 贾承造, 李德生, 等, 2005.塔里木多旋回叠合盆地的形成与演化.石油与天然气地质, 26(1):64-77. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=syyt200501009&dbname=CJFD&dbcode=CJFQ
[57] 何登发, 周新源, 张朝军, 等, 2007.塔里木地区奥陶纪原型盆地类型及其演化.科学通报, 52(增刊Ⅰ):126-135. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=kxtb2007s1015&dbname=CJFD&dbcode=CJFQ
[58] 黄宝春, 周烑秀, 朱日祥, 2008.从古地磁研究看中国大陆形成与演化过程.地学前缘, 15(3):348-359. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dxqy200803034&dbname=CJFD&dbcode=CJFQ
[59] 贾承造, 1997.中国塔里木盆地构造特征与油气.北京:石油工业出版社.
[60] 康磊, 刘良, 曹玉亭, 等, 2011.北阿尔金构造带红柳沟钾长花岗岩地球化学特征、LA-ICP-MS锆石U-Pb定年和Hf同位素组成.地质通报, 30(7):1066-1076. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=zqyd201107008&dbname=CJFD&dbcode=CJFQ
[61] 李江海, 王洪浩, 李维波, 等, 2014.显生宙全球古板块再造及构造演化.石油学报, 35(2):207-218. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=syxb201402001&dbname=CJFD&dbcode=CJFQ
[62] 李培军, 陈红汉, 唐大卿, 等, 2017.塔里木盆地顺南地区中-下奥陶统NE向走滑断裂及其与深成岩溶作用的耦合关系.地球科学, 42(1):93-104. https://doi.org/10.3799/dqkx.2017.007
[63] 刘伟, 张兴阳, 顾家裕, 等, 2009.塔里木盆地台盆区中西部中下奥陶统鹰山组沉积环境研究.沉积学报, 27(3):435-442. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=cjxb200903007&dbname=CJFD&dbcode=CJFQ
[64] 刘忠宝, 高山林, 刘士林, 等, 2015.塔里木盆地巴楚-麦盖提地区奥陶系碳酸盐岩沉积特征及模式.中南大学学报(自然科学版), 46(11):4165-4173. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=zngd201511026&dbname=CJFD&dbcode=CJFQ
[65] 戚学祥, 李海兵, 吴才来, 等, 2005.北阿尔金恰什坎萨依花岗闪长岩的锆石SHRIMP U-Pb定年及其地质意义.科学通报, 50(6):571-576. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=kxtb20050600b&dbname=CJFD&dbcode=CJFQ
[66] 沈安江, 赵文智, 胡安平, 等, 2015.海相碳酸盐岩储集层发育主控因素.石油勘探与开发, 42(5):1-10. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=skyk201505001&dbname=CJFD&dbcode=CJFQ
[67] 史仁灯, 杨经绥, 吴才来, 等, 2004.北祁连玉石沟蛇绿岩形成于晚震旦世的SHRIMP年龄证据.地质学报, 78(5):649-657. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dzxe200405008&dbname=CJFD&dbcode=CJFQ
[68] 孙崇浩, 于红枫, 王怀盛, 等, 2012.塔里木盆地塔中地区奥陶系鹰山组碳酸盐岩孔洞发育规律研究.天然气地球科学, 23(2):230-236. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=tdkx201202006&dbname=CJFD&dbcode=CJFQ
[69] 王成林, 邬光辉, 崔文娟, 等, 2011.塔里木盆地奥陶系鹰山组台内滩的特征与分布.沉积学报, 29(6):1048-1057. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=cjxb201106005&dbname=CJFD&dbcode=CJFQ
[70] 王铁冠, 宋到福, 李美俊, 等, 2014.塔里木盆地顺南-古城地区奥陶系鹰山组天然气气源与深层天然气勘探前景.石油与天然气地质, 35(6):753-762. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=syyt201406003&dbname=CJFD&dbcode=CJFQ
[71] 吴才来, 杨经绥, 姚尚志, 等, 2005.北阿尔金巴什考供盆地南缘花岗杂岩体特征及锆石SHRIMP定年.岩石学报, 21(3):846-858. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb200503025&dbname=CJFD&dbcode=CJFQ
[72] 吴才来, 姚尚志, 曾令森, 等, 2007.北阿尔金巴什考供-斯米尔布拉克花岗岩特征及锆石SHRIMP U-Pb定年.中国科学:地球科学, 37(1):10-26. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=jdxk200701001&dbname=CJFD&dbcode=CJFQ
[73] 吴兴宁, 斯春松, 俞广, 等, 2012.塔里木盆地奥陶纪岩相古地理恢复及其油气勘探意义.海相油气地质, 17(3):9-17. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=hxyq201203004&dbname=CJFD&dbcode=CJFQ
[74] 肖文交, 侯泉林, 李继亮, 等, 2000.西昆仑大地构造相解剖及其多岛增生过程.中国科学:地球科学, 30(增刊):22-28. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=jdxk2000s1003&dbname=CJFD&dbcode=CJFQ
[75] 肖序常, 王军, 苏梨, 等, 2003.再论西昆仑库地蛇绿岩及其构造意义.地质通报, 22(10):745-750. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=zqyd200310000&dbname=CJFD&dbcode=CJFQ
[76] 熊剑飞, 余腾孝, 曹自成, 等, 2013.塔里木盆地奥陶系"鹰山组"的解体及中下统界线的划分.地层学杂志, 37(3):283-291. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dcxz201303005&dbname=CJFD&dbcode=CJFQ
[77] 修群业, 于海峰, 刘永顺, 等, 2007.阿尔金北缘枕状玄武岩的地质特征及其锆石U-Pb年龄.地质学报, 81(6):787-794. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dzxe200706005&dbname=CJFD&dbcode=CJFQ
[78] 徐向珍, 杨经绥, 郭国林, 等, 2011.新疆天山地区榆树沟-铜花山蛇绿岩特征和构造背景.岩石学报, 27(1):96-120. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb201101007&dbname=CJFD&dbcode=CJFQ
[79] 许效松, 汪正江, 万方, 等, 2005.塔里木盆地早古生代构造古地理演化与烃源岩.地学前缘, 12(3):49-57. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dxqy200503007&dbname=CJFD&dbcode=CJFQ
[80] 许志琴, 李思田, 张建新, 等, 2011.塔里木地块与古亚洲/特提斯构造体系的对接.岩石学报, 27(1):1-22. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb201101002&dbname=CJFD&dbcode=CJFQ
[81] 严威, 王兴志, 王振宇, 等, 2010.塔中及相邻地区早奥陶世沉积格局新论.沉积学报, 28(6):1090-1097. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=cjxb201006007&dbname=CJFD&dbcode=CJFQ
[82] 杨经绥, 史仁灯, 吴才来, 等, 2008.北阿尔金地区米兰红柳沟蛇绿岩的岩石学特征和SHRIMP定年.岩石学报, 24(7):1567-1584. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb200807014&dbname=CJFD&dbcode=CJFQ
[83] 杨经绥, 徐向珍, 李天福, 等, 2011.新疆中天山南缘库米什地区蛇绿岩的锆石U-Pb同位素定年:早古生代洋盆的证据.岩石学报, 27(1):77-95. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb201101006&dbname=CJFD&dbcode=CJFQ
[84] 尹得功, 郑玉壮, 弓小平, 等, 2013.西昆仑库地岩组地质特征及形成时代.新疆地质, 31(4):281-286. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=xjdi201304003&dbname=CJFD&dbcode=CJFQ
[85] 于炳松, 林畅松, 樊太亮, 等, 2011.塔里木盆地寒武纪-奥陶纪区域地球动力学转换的沉积作用响应及其储层地质意义.地学前缘, 18(3):221-232. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201503025.htm
[86] 张丽娟, 李勇, 周成刚, 等, 2007.塔里木盆地奥陶纪岩相古地理特征及礁滩分布.石油与天然气地质, 28(6):731-737. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=syyt200706006&dbname=CJFD&dbcode=CJFQ
[87] 赵文智, 沈安江, 潘文庆, 等, 2013.碳酸盐岩岩溶储层类型研究及对勘探的指导意义-以塔里木盆地岩溶储层为例.岩石学报, 29(9):3213-3222. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb201309020&dbname=CJFD&dbcode=CJFQ
[88] 赵宗举, 吴兴宁, 潘文庆, 等, 2009.塔里木盆地奥陶纪层序岩相古地理.沉积学报, 27(5):939-955. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=cjxb200905019&dbname=CJFD&dbcode=CJFQ