Permian very low-grade metamorphism and its potential for hydrocarbon generation in the Linxi-Wulanhaote Area, Inner Mongolia, China
-
摘要: 极低级变质作用对年轻造山带构造演化和油气勘探有重要意义,近年来成为地质学家探讨的热点领域。文章以中国东北地区南缘石炭—二叠系为研究对象,探讨了其极低级变质作用的特征。通过对兴蒙造山带东段林西—乌兰浩特地区二叠纪地层的伊利石结晶度、b0值和多型等参数进行测试分析发现,伊利石结晶度Kübler指数在0.175~0.47之间,大多数集中于0.25~0.35,平均值为0.30;样品b0值主要在9.0155~9.0316 Å之间,平均值为9.0249 Å;伊利石多型主要为2M1。以上结果表明研究区二叠系林西组和哲斯组主要经历了葡萄石-绿纤石相的极低级变质作用,变质温度200~370 ℃,压力为中压,同时表明其具有较高的生烃潜力。结合二叠系生烃期研究和区内广泛发育的白垩纪侵入体推测,二叠系极低级变质作用可能发生在早白垩世,且与岩体侵入导致的地温梯度升高有关。Abstract: The very low-grade metamorphism has been the focus of research in recent years and has great significance for the study of structural evolution of young orogenic belt and petroleum exploration. The recent studies revealed that the Carboniferous Permian strata in the northeastern part of China mainly underwent very low-grade metamorphism and gradually became a new petroleum exploration layer. This paper launched studies on the illite crystallinity, illite polytype and illite b0 dimension of the Permian System in the Linxi-Wulanhaote Area. The illite crystallinity ranges from 0.175 to 0.47, mainly clustering between 0.25 and 0.35 with an average of 0.30. Illite b0 ranges from 9.0155 to 9.0316 Å, with an average of 9.0249 Å. Illite polytype is predominantly 2M1. Based on the above data, the Permian System in the study area mainly experienced the prehnite-pumpellyite facies very low-grade metamorphism under medium-pressure with metamorphic temperature at 200~370℃, indicating its potential for hydrocarbon generation. Together with the hydrocarbon generation history of the Permian strata and the widespread Cretaceous granites in the study area, the very low-grade metamorphism might occurred during the early-Cretaceous, related to the increase of geothermal gradient caused by the intrusion of granite.
-
Key words:
- very low-grade metamorphism /
- illite /
- Permian /
- Xing'an-Mongolia Orogenic Belt
-
图 1 研究区二叠系区域分布图(据胡大千和于介江,2009;李娟等,2011修改)
Figure 1. Distribution of the Permian System in the study area (modified after Hu and Yu, 2009; Li et al., 2011)
图 6 胡都格绍荣岩体地质简图(据李鹏川等,2016修改)
Figure 6. Geological sketch map of the Hudugeshaorong rock mass. (modified after Li et al., 2016)
表 1 样品矿物含量/%
Table 1. Mineral contents of the samples
序号 样品编号 石英 长石 碳酸盐 辉石 高岭石 黑云母 绿泥石 伊利石 蒙脱石 伊/蒙混层 1 LX-1 40 15 1 / 1 / 1 42 / / 2 LX-2 34 18 1 / 2 / / 45 / / 3 XM034-1 26 29 2 / 1 1 2 28 / 11 4 XM041-1 35 5 8 / 1 1 3 29 / 18 5 XM046-1 32 12 3 / / / / 5 / 48 6 XM046-2 29 14 1 / 1 / 2 20 / 33 7 XM046-3 25 20 1 / 1 / 3 21 / 29 8 XM051-1 35 34 1 / 1 1 5 14 9 / 9 XM051-3 34 16 / / 1 / 4 20 25 / 10 XM052-1 35 15 1 / 2 / 2 40 5 / 11 XM052-2 45 34 1 / / 1 / 5 4 10 12 XM052-3 28 20 2 / / / / 6 / 44 13 XM065-1 38 4 1 / 1 / / 56 / / 14 XM065-2 36 8 2 / 1 / 2 25 26 / 15 XM065-3 22 10 1 / 4 / 5 30 28 / 16 XM065-4 24 6 1 / / / / 30 39 / 17 XM066-1 34 12 1 / / / / 34 / 19 18 XM066-2 33 14 1 / 1 / / 41 / 10 19 XM078-1 32 4 2 / 2 / 1 49 10 / 20 XM080-1 / 6 10 64 / / 20 / / / 21 XM080-2 31 15 1 / 2 / 1 30 20 / 22 XM082-5 35 20 1 / 1 / / 33 10 / 23 XM0102-1 40 8 2 / 2 / / 40 8 / 24 XM0113-1 29 10 / / 5 / 2 10 / 44 表 2 样品伊利石结晶度Kübler指数、b0值和多型
Table 2. Kübler Index, b0 and polytype of the illite samples
序号 样品编号 岩性 采样层位 坐标 结晶度Kübler指数(KI°Δ2 θ) b0值/Å 多型 N E 1 LX-1 粉砂岩 林西组 43°44′26″ 118°06′38″ 0.332 9.0215 2M1 2 LX-2 粉砂岩 林西组 43°44′25″ 118°06′41″ 0.335 9.0226 2M1 3 XM034-1 变质砂岩 哲斯组 43°50′07″ 113°48′39″ 0.211 9.0285 2M1 4 XM041-1 泥岩 哲斯组 43°14′06″ 117°13′05″ 0.47 9.0155 2M1 5 XM046-1 泥岩 林西组 43°24′58″ 118°02′18″ 0.298 9.0288 2M1 6 XM046-2 泥岩 林西组 43°24′58″ 118°02′18″ 0.314 9.0223 2M1 7 XM046-3 泥岩 林西组 43°24′58″ 118°02′18″ 0.374 9.0224 2M1 8 XM051-1 泥岩 哲斯组 43°28′37″ 117°28′38″ 0.197 9.0316 2M1 9 XM051-3 泥岩 哲斯组 43°28′38″ 117°28′38″ 0.335 9.0233 2M1 10 XM052-1 泥岩 哲斯组 43°25′21″ 117°34′14″ 0.331 9.0235 2M1 11 XM052-2 泥岩 哲斯组 43°25′21″ 117°34′14″ 0.302 9.0213 2M1 12 XM052-3 泥岩 哲斯组 43°25′21″ 117°34′14″ 0.279 9.0265 2M1 13 XM065-1 泥岩 哲斯组 43°57′56″ 118°18′08″ 0.243 9.0278 2M1 14 XM065-2 泥岩 哲斯组 43°57′56″ 118°18′08″ 0.324 9.0241 2M1 15 XM065-3 泥岩 哲斯组 43°57′56″ 118°18′08″ 0.347 9.0213 2M1 16 XM065-4 泥岩 哲斯组 43°57′56″ 118°18′08″ 0.377 9.0211 2M1 17 XM066-1 泥岩 林西组 43°47′51″ 118°15′45″ 0.388 9.0221 2M1 18 XM066-2 泥岩 林西组 43°47′51″ 118°15′45″ 0.305 9.0266 2M1 19 XM078-1 泥岩 哲斯组 44°28′09″ 117°28′20″ 0.293 9.0281 2M1 20 XM080-1 泥岩 林西组 44°21′29″ 118°02′18″ / / / 21 XM080-2 泥岩 林西组 44°21′29″ 118°02′18″ 0.321 9.0255 2M1 22 XM082-5 泥岩 林西组 44°23′06″ 118°10′33″ 0.175 9.0315 2M1 23 XM102-1 泥岩 林西组 46°10′56″ 121°28′60″ 0.203 9.0288 2M1 24 XM113-1 泥岩 林西组 46°25′21″ 122°21′03″ 0.247 9.0279 2M1 -
AN J L, WANG H J, YUAN L, 2018. Very low-grade metamorphism of the Precambrian along profile Kaili-Rongjiang-Congjiang in southeastern Guizhou Province, China[J]. Acta Petrologica Sinica, 34(3):669-684. (in Chinese with English abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201803009 CHU H, ZHANG J R, WEI C J, et al., 2013. A new interpretation of the tectonic setting and age of meta-basic volcanics in the Ondor Sum Group, Inner Mongolia[J]. Chinese Science Bulletin, 58(28-29):3580-3587. doi: 10.1007/s11434-013-5862-7 DONG S B, SHEN Q H, SUN D Z, et al., 1986. Metamorphic map of China[M]. Beijing:Geological Publishing House:1-37. (in Chinese) DUAN Z, XING G F, YU M G, et al., 2018. Very low-grade metamorphism of Early Cretaceous volcanic rocks in the Southeast Coastal of China[J]. Acta Petrologica Sinica, 34(3):656-668. (in Chinese with English abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201803008 FERREIRO MÄHLMANN R, BOZKAYA Ö, POTEL S, et al., 2012. The pioneer work of Bernard Kübler and Martin Frey in very low-grade metamorphic terranes: paleo-geothermal potential of variation in Kübler-Index/organic matter reflectance correlations. A review[J]. Swiss Journal of Geosciences, 105(2): 121-152. FREY M, ROBINSON D, 1999. Low-grade metamorphism[M]. Oxford:Blackwell Science:10-226. GUIDOTTI C V, SASSI F P, 1986. Classification and correlation of metamorphic facies series by means of muscovite B0 data from low-grade metapelites[J]. Neues Jahrbuch fur Mineralogie Abhandlungen, 153:363-380. HU D Q, HONG Y, YU J J, 2010a. Genetic chariciterics of illite in the carboniferous- permian pelitic rocks in east Jilin province[J]. Journal of Jilin University (Earth Science Edition), 40(5):1035-1040. (in Chinese with English abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cckjdxxb201005008 HU D Q, WANG X W, YU J J, 2010b. Study of late-permian diagenetic-very low metamorphic mineral in East of Inner Mongolia[J]. Acta Mineralogica Sinica, 30(S1):91. (in Chinese with English abstract) HU D Q, WANG Y Q, SHA Q, et al., 2015. Very low grade metamorphic temperatures of the upper paleozoic strata in northern Daxing'Anling area, NE China:evidence from Raman spectrum studies of carbonaceous materials[J]. Journal of Jilin University (Earth Science Edition), 45(1):188-197. (in Chinese with English abstract) HU D Q, YU J J, 2009. Study of illite in the upper Paleozoic, in northeastern Inner Mongolia[J]. Acta Petrologica Sinica, 25(8):2017-2022. (in Chinese with English abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200908025 HU L, LIU J L, JI M, et al., 2009. Instructions for identification of deformation and microstructures[M]. Beijing:Geological Publishing House:41-73. (in Chinese). KANG Y Z, XING S W, LI H J, et al., 2019. Features of structural systems in northern China and its control on basin and hydrocarbon distribution[J]. Journal of Geomechanics, 25(6):1013-1024. (in Chinese with English abstract) http://d.old.wanfangdata.com.cn/Periodical/dzlxxb201906002 KISCH H J, 1991. Development of slaty cleavage and degree of very-low-grade metamorphism:a review[J]. Journal of Metamorphic Geology, 9(6):735-750. doi: 10.1111/j.1525-1314.1991.tb00562.x KÜBLER B, 1967. La cristallinité de l'illite à les zones tout a fait supérieures du métamorphismé[M]//Étages tectoniques. Neuchatel, Switzerland: A La Baconnière: 105-121. LI J, ZHENG C Q, JIN W, et al., 2011. A study of contact metamorphism of late paleozoic strata in the middle of Inner Mongolia[J]. Earth Science Frontiers, 18(2):223-230. (in Chinese with English abstract) http://d.old.wanfangdata.com.cn/Periodical/dxqy201102019 LI P C, LIU Z H, LI S C, et al., 2016. Geochronology, geochemistry, Zircon Hf isotopic characteristics and tectonic setting of hudugeshaorong pluton in Balinyouqi, Inner Mongolia[J]. Earth Science, 41(12):1995-2007. (in Chinese with English abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201612002 MERRIMAN R J, 1991. Phyllosilicates as indicators of very low-grade metamorphism and diagenesis:introduction[J]. Journal of Metamorphic Geology, 9(6):663-664. doi: 10.1111/j.1525-1314.1991.tb00555.x REN Z L, XIAO D M, CHI Y L, 2006. Research on the gas-generatingstage of the source rocks in the Carboniferous-Permian basement, Songliao basin, China[J]. Progress in Natural Science, 16(8):974-979. (in Chinese with English abstract) SHEN Q H, GENG Y S, SONG H X, 2018. Strengthening the study of very low-grade metamorphism[J]. Acta Petrologica et Mineralogica, 37(2):342-348. (in Chinese with English abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=yskwxzz201802013 SU F, LI Z, ZHANG J, et al., 2017. Discovery of the soure rock from upper Permain Linxi Formation in Tuquan Basin, Inner Mongolia[J]. Geology and Resources, 26(3):268-274. (in Chinese with English abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gjsdz201703009 SUN P, TANG Y J, ZHANG Y S, et al., 2016. The characteristics of biomarker compounds of source rocks in linxi formation in Guandi section of linxi county in the east of Inner Mongolia[J]. Journal of Yangtze University (Natural Science Edition), 13(32):1-6. (in Chinese with English abstract) SUO S T, BI X M, ZHAO W X, et al., 1998. Very low grade metamorphism and its geodynamical significance of Triassic strata within the Youjiang River basin[J]. Scientia Geologica Sinica, 33(4):395-405. (in Chinese with English abstract) TANG Y J, MA Z M, JIANG X C, 2013. Characteristics and significance of biomarker compounds of Linxi Formation hydrocarbon source rocks along Taohaiyingzi section in Zhalute basin, Inner Mongolia[J]. Geological Bulletin of China, 32(8):1315-1321. (in Chinese with English abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgqydz201308019 WANG C W, JIN W, ZHANG X Z, et al., 2008. New understanding of the late Paleozoic tectonics in northeastern China and adjacent areas[J]. Journal of Stratigraphy, 32(2):119-136. (in Chinese with English abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dcxzz200802001 WANG C W, SUN Y W, LI N, et al., 2009. On the distribution of Late Palaeozoic strata in northeast China[J]. Journal of Startigraphy, 33(1):56-61. (in Chinese with English abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dcxzz200901006 WANG H J, ZHOU J, 1998. On the indices of illite crystallinity[J]. Acta Petrologica Sinica, 14(3):395-405. (in Chinese with English abstract) WU F Y, SUN D Y, GE W C, et al., 2011. Geochronology of the phanerozoic granitoids in northeastern China[J]. Journal of Asian Earth Sciences, 41(1):1-30. doi: 10.1016/j.jseaes.2010.11.014 WU H Q, TIAN B, LIU Y Q, 1994. Very low-grade metamorphism: mechanisms and geological applications[C]//Proceedings of IGCP294 international symposium. YAO J, HU D Q, SUN G S, et al., 2016. Raman spectrum characteristics of organic materials of Middle Permian Zhesi Formation in Suolun area, Inner Mongolia and their geological implication[J]. Global Geology, 35(3):760-770. (in Chinese with English abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=sjdz201603016 YU H Z, CAI X Y, HAN S H, et al., 2003. The carboniferous-permian source rocks in the Songliao basin[J]. Sedimentary Geology and Tethyan Geology, 23(2):62-66. (in Chinese with English abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=yxgdl200302012 YU J J, HU D Q, ZHANG J H, 2012. Genetic chariciterics of the illite from the upper paleozoic group in Heilongjiang province and its geological significance[J]. Journal of Jilin University (Earth Science Edition), 42(6):1817-1824. (in Chinese with English abstract) YUAN Y M, SANG L K, LI D W, et al., 2008. Low-very low-grade metamorphism of the Hoh xil triassic Bayanhar group on Qinghai-Tibet plateau[J]. Geological Science and Technology Information, 27(3):14-20. (in Chinese with English abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzkjqb200803002 ZHANG J, BIAN X F, SU F, et al., 2013. Evaluation on hydrocarbon genetic potential of linxi formation of upper permian in well Lu D1 in zhalute area of Inner Mongolia[J]. Journal of Oil and Gas Technology, 35(10):63-67. (in Chinese with English abstract) ZHANG J R, WEI C J, CHU H, 2015. Blueschist metamorphism and its tectonic implication of Late Paleozoic-Early Mesozoic metabasites in the mélange zones, central Inner Mongolia, China[J]. Journal of Asian Earth Sciences, 97:352-364. ZHANG J R, WEI C J, CHU H, 2016. Mesozoic metamorphism and its tectonic implication along the Solonker suture zone in central Inner Mongolia, China[J]. Lithos, 261:262-277. doi: 10.1016/j.lithos.2016.03.014 ZHANG J R, WEI C J, CHU H, 2018. Multiple metamorphic events recorded in the metamorphic terranes in central Inner Mongolia, Northern China:implication for the tectonic evolution of the Xing'an-Inner Mongolia Orogenic Belt[J]. Journal of Asian Earth Sciences, 167:52-67. doi: 10.1016/j.jseaes.2018.04.007 ZHANG L F, 1994. The research advances of illite crystallite[J]. Earth Science Frontiers, (Z1):201-202. (in Chinese) ZHANG L F, 2007. Extreme metamorphism:the frontier of metamorphic geology[J]. Earth Science Frontiers, 14(1):33-42. (in Chinese with English abstract) ZHANG L Y, SONG L C, LI H J, et al., 2019. The role of geomechanics theory in the exploration of deep oil and gas in China[J]. Journal of Geomechanics, 25(6):1036-1047. (in Chinese with English abstract) http://d.old.wanfangdata.com.cn/Periodical/dzlxxb201906004 ZHANG X Z, MA Y X, CHI X G, et al., 2012. Discussion on phanerozoic tectonic evolution in northeastern China[J]. Journal of Jilin University (Earth Science Edition), 42(5):1269-1285. (in Chinese with English abstract) ZHANG X Z, QIAO D W, CHI X G, et al., 2011. Late-Paleozoic tectonic evolution and oil-gas potential in northeastern China[J]. Geological Bulletin of China, 30(2-3):205-213. (in Chinese with English abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgqydz201102004 ZHANG X Z, ZHOU J B, CHI X G, et al., 2008. Late paleozoic tectonic-sedimentation and petroleum resources in northeastern China[J]. Journal of Jilin University (Earth Science Edition), 38(5):719-725. (in Chinese with English abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cckjdxxb200805001 安佳丽, 王河锦, 苑蕾, 2018.黔东南凯里-榕江-从江前寒武系甚低级变质作用研究[J].岩石学报, 34(3):669-684. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201803009 董申保, 沈其韩, 孙大中, 等. 1986.中国变质地质图 1:4000000说明书[M].北京:地质出版社:1-37. 段政, 邢光福, 余明刚, 等, 2018.东南沿海早白垩世火山岩的极低级变质作用研究[J].岩石学报, 34(3):656-668. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201803008 胡大千, 于介江, 2009.内蒙古东北地区上古生界伊利石研究[J].岩石学报, 25(8):2017-2022. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200908025 胡大千, 洪艳, 于介江, 2010a.吉林省东部石炭-二叠系伊利石的成因标志[J].吉林大学学报(地球科学版), 40(5):1035-1040. http://d.old.wanfangdata.com.cn/Periodical/cckjdxxb201005008 胡大千, 王秀文, 于介江, 2010b.内蒙古东部晚古生代区域成岩-极低级变质矿物研究[J].矿物学报, 30(S1):91. http://www.cnki.com.cn/Article/CJFDTotal-KWXB2010S1053.htm 胡大千, 王岩泉, 沙茜, 等, 2015.大兴安岭北部上古生界极低级变质温度:来自碳质物拉曼光谱的证据[J].吉林大学学报(地球科学版), 45(1):188-197. http://d.old.wanfangdata.com.cn/Periodical/cckjdxxb201501018 胡玲, 刘俊来, 纪沫, 等, 2009.变形显微构造识别手册[M].北京:地质出版社:41-73. 康玉柱, 邢树文, 李会军, 等, 2019.中国北方地区构造体系控盆作用与控油分布规律[J].地质力学学报, 25(6):1013-1024. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?file_no=20190602&flag=1 李娟, 郑常青, 金巍, 等, 2011.内蒙古中部地区晚古生代地层接触变质作用研究初探[J].地学前缘, 18(2):223-230. http://d.old.wanfangdata.com.cn/Periodical/dxqy201102019 李鹏川, 刘正宏, 李世超, 等, 2016.内蒙古巴林右旗胡都格绍荣岩体的年代学、地球化学、Hf同位素特征及构造背景[J].地球科学, 41(12):1995-2007. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201612002 任战利, 萧德铭, 迟元林, 2006.松辽盆地基底石炭-二叠系烃源岩生气期研究[J].自然科学进展, 16(8):974-979. doi: 10.3321/j.issn:1002-008X.2006.08.009 沈其韩, 耿元生, 宋会侠, 2018.加强极低级变质作用研究[J].岩石矿物学杂志, 37(2):342-348. doi: 10.3969/j.issn.1000-6524.2018.02.013 苏飞, 李臻, 张健, 等, 2017.内蒙古突泉盆地突D2井上二叠统林西组烃源岩新发现[J].地质与资源, 26(3):268-274. http://d.old.wanfangdata.com.cn/Periodical/gjsdz201703009 孙鹏, 唐友军, 张永生, 等, 2016.林西县官地剖面林西组烃源岩生物标志化合物特征[J].长江大学学报(自科版), 13(32):1-6. doi: 10.3969/j.issn.1673-1409(s).2016.32.002 索书田, 毕先梅, 赵文霞, 等, 1998.右江盆地三叠纪岩层极低级变质作用及地球动力学意义[J].地质科学, 33(4):395-405. doi: 10.3321/j.issn:0563-5020.1998.04.002 唐友军, 马忠梅, 蒋兴超, 2013.内蒙古扎鲁特盆地陶海营子剖面林西组烃源岩生物标志化合物特征及意义[J].地质通报, 32(8):1315-1321. doi: 10.3969/j.issn.1671-2552.2013.08.019 王成文, 金巍, 张兴洲, 等, 2008.东北及邻区晚古生代大地构造属性新认识[J].地层学杂志, 32(2):119-136. doi: 10.3969/j.issn.0253-4959.2008.02.001 王成文, 孙跃武, 李宁, 等, 2009.东北地区晚古生代地层分布规律[J].地层学杂志, 33(1):56-61. doi: 10.3969/j.issn.0253-4959.2009.01.006 王河锦, 周健, 1998.关于伊利石结晶度诸指数的评价[J].岩石学报, 14(3):395-405. http://d.old.wanfangdata.com.cn/Periodical/ysxb98199803013 姚杰, 胡大千, 孙国胜, 等, 2016.内蒙古索伦地区中二叠统哲斯组有机质的拉曼光谱特征及地质意义[J].世界地质, 35(3):760-770. doi: 10.3969/j.issn.1004-5589.2016.03.016 余和中, 蔡希源, 韩守华, 等, 2003.松辽盆地石炭-二叠系烃源岩研究[J].沉积与特提斯地质, 23(2):62-66. doi: 10.3969/j.issn.1009-3850.2003.02.012 于介江, 胡大千, 张嘉惠, 2012.黑龙江省上古生界伊利石的成因标志及其地质意义[J].吉林大学学报(地球科学版), 42(6):1817-1824. http://www.cnki.com.cn/Article/CJFDTotal-CCDZ201206025.htm 袁晏明, 桑隆康, 李德威, 等, 2008.青藏高原可可西里地区三叠系巴彦喀拉山群低级-极低级变质作用[J].地质科技情报, 27(3):14-20. doi: 10.3969/j.issn.1000-7849.2008.03.002 张健, 卞雄飞, 苏飞, 等, 2013.内蒙古扎鲁特地区鲁D1井上二叠统林西组生烃潜力研究[J].石油天然气学报, 35(10):63-67. doi: 10.3969/j.issn.1000-9752.2013.10.014 张立飞, 1994.伊利石结晶度研究进展之二[J].地学前缘, (Z1):201-202. http://www.cnki.com.cn/Article/CJFDTotal-DXQY4Z1.041.htm 张立飞, 2007.极端条件下的变质作用:变质地质学研究的前沿[J].地学前缘, 14(1):33-42. doi: 10.3321/j.issn:1005-2321.2007.01.003 张林炎, 宋立才, 李会军, 等, 2019.地质力学理论对中国深层油气勘查的作用[J].地质力学学报, 25(6):1036-1047. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?file_no=20190604&flag=1 张兴洲, 周建波, 迟效国, 等, 2008.东北地区晚古生代构造-沉积特征与油气资源[J].吉林大学学报(地球科学版), 38(5):719-725. http://d.old.wanfangdata.com.cn/Periodical/cckjdxxb200805001 张兴洲, 乔德武, 迟效国, 等, 2011.东北地区晚古生代构造演化及其石油地质意义[J].地质通报, 30(2-3):205-213. http://d.old.wanfangdata.com.cn/Periodical/zgqydz201102004 张兴洲, 马玉霞, 迟效国, 等, 2012.东北及内蒙古东部地区显生宙构造演化的有关问题[J].吉林大学学报(地球科学版), 42(5):1269-1285. http://www.cnki.com.cn/Article/CJFDTotal-CCDZ201205003.htm