川南茅一段白云石化过程及对眼球状灰岩形成的指示——以DB1井为例

田辰; 胡广; 徐政语; 庞谦; 刘人萍; 刘沛云; 刘屹东; 田辰; 胡广; 徐政语; 庞谦; 刘人萍; 刘沛云; 刘屹东

doi:10.14027/j.issn.1000-0550.2024.045

[1]

陈武，季寿元. 1985. 矿物学导论[M]. 北京：地质出版社：1-297.

Chen Wu, Ji Shouyuan. 1985. An introdluction to mineralogy[M]. Beijing: Geological Publishing House: 1-297.

[2]

陈轩，赵文智，张利萍，等. 2012. 川中地区中二叠统构造热液白云岩的发现及其勘探意义[J]. 石油学报，33（4）：562-569.

Chen Xuan, Zhao Wenzhi, Zhang Liping, et al. 2012. Discovery and exploration significance of structure-controlled hydrothermal dolomites in the Middle Permian of the central Sichuan Basin[J]. Acta Petrolei Sinica, 33(4): 562-569.

[3]

冯增昭，王英华，刘焕杰，等. 1994. 中国沉积学[M]. 北京：石油工业出版社：1- 968.

Feng Zengzhao, Wang Yinghua, Liu Huanjie, et al. 1994. Sedimentology of China[M]. Beijing: Petroleum Industry Press: 1-968.

[4]

韩月卿，郝运轻，韩文彪，等. 2022. 川东南地区中二叠统茅口组一段眼球状灰岩成因机理[J]. 油气地质与采收率，29（6）：12-21.

Han Yueqing, Hao Yunqing, Han Wenbiao, et al. 2022. Genetic mechanism of eyeball-shaped limestone in First member of Middle Permian Maokou Formation in southeast Sichuan Basin[J]. Petroleum Geology and Recovery Efficiency, 29(6): 12-21.

[5]

何明薇，罗进雄. 2016. 湖北兴山峡口中二叠统眼球状石灰岩特征及成因[J]. 长江大学学报（自科版），13（14）：1-8.

He Mingwei, Luo Jinxiong. 2016. Origin and characteristics of Middle Permian eyeball-shaped limestone in Xiakou area of Xingshan county of Hubei province[J]. Journal of Yangtze University (Natural Science Edition), 13(14): 1-8.

[6]

赫云兰，刘波，秦善. 2010. 白云石化机理与白云岩成因问题研究[J]. 北京大学学报（自然科学版），46（6）：1010-1020.

He Yunlan, Liu Bo, Qin Shan. 2010. Study on the dolomitization and dolostone genesis[J]. Acta Scientiarum Naturalium Universitatis Pekinensis, 46(6): 1010-1020.

[7]

何溥为，胥旺，张连进，等. 2021. 川中磨溪—高石梯地区栖霞组白云岩特征及成因机制[J]. 沉积学报，39（6）：1532-1545.

He Puwei, Xu Wang, Zhang Lianjin, et al. 2021. Characteristics and genetic mechanism of Qixia Formation dolomite in Moxi-Gaoshiti area, central Sichuan Basin[J]. Acta Sedimentologica Sinica, 39(6): 1532-1545.

[8]

胡东风，王良军，黄仁春，等. 2019. 四川盆地东部地区中二叠统茅口组白云岩储层特征及其主控因素[J]. 天然气工业，39（6）：13-21.

Hu Dongfeng, Wang Liangjun, Huang Renchun, et al. 2019. Characteristics and main controlling factors of the Middle Permian Maokou dolomite reservoirs in the eastern Sichuan Basin[J]. Natural Gas Industry, 39(6): 13-21.

[9]

胡明毅，胡忠贵，魏国齐，等. 2012. 四川盆地茅口组层序岩相古地理特征及储集层预测[J]. 石油勘探与开发，39（1）：45-55.

Hu Mingyi, Hu Zhonggui, Wei Guoqi, et al. 2012. Sequence lithofacies paleogeography and reservoir prediction of the Maokou Formation in Sichuan Basin[J]. Petroleum Exploration and Development, 39(1): 45-55.

[10]

胡文碹，陈琪，王小林，等. 2010. 白云岩储层形成演化过程中不同流体作用的稀土元素判别模式[J]. 石油与天然气地质，2010，31（6）：810-818.

Hu Wenxuan, Chen Qi, Wang Xiaolin, et al. 2010. REE models for the discrimination of fluids in the formation and evolution of dolomite reservoirs[J]. Oil & Gas Geology, 31(6): 810-818.

[11]

黄思静. 1997. 上扬子地台区晚古生代海相碳酸盐岩的碳、锶同位素研究[J]. 地质学报，71（1）：45-53.

Huang Sijing. 1997. A study on carbon and strontium isotopes of Late Paleozoic carbonate rocks in the Upper Yangtze Platform[J]. Acta Geologica Sinica, 71(1): 45-53.

[12]

黄思静，卿海若，胡作维，等. 2008. 川东三叠系飞仙关组碳酸盐岩的阴极发光特征与成岩作用[J]. 地球科学：中国地质大学学报，33（1）：26-34.

Huang Sijing, Hairuo Qing, Hu Zuowei, et al. 2008. Cathodoluminescence and diagenesis of the carbonate rocks in Feixianguan Formation of Triassic, eastern Sichuan Basin of China[J]. Earth Science: Journal of China University of Geosciences, 33(1): 26-34.

[13]

李大军，陈辉，陈洪德，等. 2016. 四川盆地中二叠统茅口组储层形成与古构造演化关系[J]. 石油与天然气地质，37（5）：756-763.

Li Dajun, Chen Hui, Chen Hongde, et al. 2016. Relationship between reservoir development in the Middle Permian Maokou Formation and paleostructure evolution in the Sichuan Basin[J]. Oil & Gas Geology, 37(5): 756-763.

[14]

梁兴，徐政语，栗维民，等. 2023. 蜀南—渝西地区中二叠统茅一段灰质源岩气储层特征及主控因素：以DB1井为例[J]. 石油实验地质，45（4）：714-725.

Liang Xing, Xu Zhengyu, Li Weimin, et al. 2023. Characteristics and main controlling factors of the limy source rock gas reservoir in the First member of the Middle Permian Maokou Formation in the southern Sichuan and western Chongqing area: A case study of well DB 1[J]. Petroleum Geology & Experiment, 45(4): 714-725.

[15]

刘瑾，夏文谦，李晶晶，等. 2019. 川东南地区茅一段储层特征分析[J]. 科技通报，35（7）：26-32.

Liu Jin, Xia Wenqian, Li Jingjing, et al. 2019. Analysis of reservoir characteristics of the First member of Maokou Formation in southeastern Sichuan Basin[J]. Bulletin of Science and Technology, 35(7): 26-32.

[16]

刘喜停，颜佳新，马志鑫，等. 2014. 华南栖霞组灰岩—泥灰岩韵律层的成因[J]. 地球科学：中国地质大学学报，39（2）：155-164.

Liu Xiting, Yan Jiaxin, Ma Zhixin, et al. 2014. Origination of limestone-marl alternations from Qixia Formation of South China[J]. Earth Science: Journal of China University of Geosciences, 39(2): 155-164.

[17]

罗进雄，何幼斌. 2010. 中—上扬子地区二叠系眼球状石灰岩特征及成因研究[J]. 地质论评，56（5）：629-637.

Luo Jinxiong, He Youbin. 2010. Origin and characteristics of Permian eyeball-shaped limestones in Middle-Upper Yangtze region[J]. Geological Review, 56(5): 629-637.

[18]

罗进雄，何幼斌. 2014. 中上扬子地区二叠系烃源岩特征[J]. 天然气地球科学，25（9）：1416-1425.

Luo Jinxiong, He Youbin. 2014. Characteristics of the Permian source rocks in the Middle and Upper Yangtze region[J]. Natural Gas Geoscience, 5(9): 1416-1425.

[19]

罗进雄，何幼斌，何明薇，等. 2019. 华南中二叠统眼球状石灰岩特征及成因的思考[J]. 古地理学报，21（4）：613-626.

Luo Jinxiong, He Youbin, He Mingwei, et al. 2019. Thoughts on characteristics and origin of the Middle Permian eyeball-shaped limestone in South China[J]. Journal of Palaeogeography, 21(4): 613-626.

[20]

任海侠，林小兵，刘叶，等. 2021. 川西南二叠系茅口组一段滑石特征及其形成机理：以A1井茅一段样品为例[J]. 石油实验地质，43（6）：1038-1047.

Ren Haixia, Lin Xiaobing, Liu Ye, et al. 2021. Characteristics and formation mechanism of talc in Permian Maokou Formation, southwestern Sichuan Basin: A case study of First member of Maokou Formation in well A1[J]. Petroleum Geology & Experiment, 43(6): 1038-1047.

[21]

任梦怡，江青春，汪泽成，等. 2020. 川南地区中二叠统茅口组成岩流体来源及演化过程[J]. 天然气工业，40（4）：40-50.

Ren Mengyi, Jiang Qingchun, Wang Zecheng, et al. 2020. Source and evolution of diagenetic fluid in the Middle Permian Maokou Formation in the southern Sichuan Basin[J]. Natural Gas Industry, 40(4): 40-50.

[22]

宋翠玉，吕大炜. 2022. 米兰科维奇旋回时间序列分析法研究进展[J]. 沉积学报，40（2）：380-395.

Song Cuiyu, Dawei Lü. 2022. Advances in time series analysis methods for Milankovitch cycles[J]. Acta Sedimentologica Sinica, 40(2): 380-395.

[23]

唐雨，张云峰，胡林辉，等. 2021. 开江—梁平海槽西侧中东段长兴组台缘储层特征及差异性[J]. 沉积学报，2021，39（6）：1593-1608.

Tang Yu, Zhang Yunfeng, Hu Linhui, et al. 2021. Characteristics and differences of the platform margin reservoir, Changxing Formation, central eastern region, west of the Kaijiang-Liangping trough[J]. Acta Sedimentologica Sinica, 39(6): 1593-1608.

[24]

王良军，李红，曾韬，等. 2022. 四川盆地东部茅口组白云岩成因：来自岩石学、矿物学和地球化学的证据[J]. 古地理学报，24（5）：989-1016.

Wang Liangjun, Li Hong, Zeng Tao, et al. 2022. Origins of dolostones of the Maokou Formation in eastern Sichuan Basin: Evidence from lithology, mineralogy, and geochemistry[J]. Journal of Palaeogeography, 24(5): 989-1016.

[25]

向娟，胡明毅，胡忠贵，等. 2011.四川盆地中二叠统茅口组沉积相分析[J]. 石油地质与工程，25（1）：14-19.

Xiang Juan, Hu Mingyi, Hu Zhonggui, et al. 2011.Sedimentary facies analysis of Maokou Formation of Middle Permian in Sichuan Basin[J]. Petroleum Geology and Engineering, 25(1): 14-19.

[26]

许国明，谢刚平，隆轲，等. 2015. 四川盆地西南部中二叠统沉积特征与勘探目标[J]. 天然气工业，35（7）：27-33.

Xu Guoming, Xie Gangping, Long Ke, et al. 2015. Sedimentary features and exploration targets of Middle Permian reservoirs in the southwestern Sichuan Basin[J]. Natural Gas Industry, 35(7): 27-33.

[27]

薛武强，刘喜停，颜佳新，等. 2015. 重庆南川地区中二叠统茅口组眼球状灰岩成因[J]. 地质科学，50（3）：1001-1013.

Xue Wuqiang, Liu Xiting, Yan Jiaxin, et al. 2015. The origin of eyeball-shaped limestone from Maokou Formation (Mid-Permian) in Nanchuan region, Chongqing, Southwest China[J]. Chinese Journal of Geology, 50(3): 1001-1013.

[28]

于春勇，崔军平，王起琮，等. 2020. 鄂尔多斯盆地南部奥陶系马家沟组中下组合白云岩稀土元素特征及其成因[J]. 西北大学学报（自然科学版），50（5）：819-830.

Yu Chunyong, Cui Junping, Wang Qicong, et al. 2020. The REE characteristics and genesis of the middle and lower combinations dolomite of Ordovician Majiagou in the southern Ordos Basin[J]. Journal of Northwest University (Natural Science Edition), 50(5): 819-830.

[29]

张宝民，单秀琴，张静，等. 2017. 中国海相碳酸盐岩储层地质与成因[M]. 北京：科学出版社：1- 617.

Zhang Baomin, Shan Xiuqin, Zhang Jing, et al. 2017. Geology and genesis of marine carbonate reservoirs in China[M]. Beijing: Science Press: 1-617.

[30]

张涛，苏玉山，佘刚，等. 2015. 热液白云岩发育模式：以扎格罗斯盆地白垩系A油田为例[J]. 石油与天然气地质，36（3）：393-401.

Zhang Tao, Su Yushan, She Gang, et al. 2015. A study on the genetic model of hydrothermal dolomitization in Taq Taq oilfield, Kurdistan region, Iraq—taking oilfield A in the Cretaceous in Zagros Basin as an example[J]. Oil & Gas Geology, 36(3): 393-401.

[31]

张玺华，陈聪，黄婕，等. 2019. 四川盆地中二叠世广元—巴中拉张槽的发现及其油气地质意义[J]. 中国石油勘探，24（4）：466-475.

Zhang Xihua, Chen Cong, Huang Jie, et al. 2019. The discovery of Middle Permian Guangyuan-Bazhong extensional trough in the Sichuan Basin and its petroleum geological significance[J]. China Petroleum Exploration, 24(4): 466-475.

[32]

张玺华，陈聪，张亚，等. 2018. 川西北地区茅口组海槽相地质特征及其油气地质意义[J]. 天然气勘探与开发，41（3）：42-50.

Zhang Xihua, Chen Cong, Zhang Ya, et al. 2018. Geological characteristics of trough facies, Maokou Formation, northwestern Sichuan Basin: Implications for geology[J]. Natural Gas Exploration and Development, 41(3): 42-50.

[33]

Bau M. 1996. Controls on the fractionation of isovalent trace elements in magmatic and aqueous systems: Evidence from Y/Ho, Zr/Hf, and lanthanide tetrad effect[J]. Contributions to Mineralogy and Petrology, 123(3): 323-333.

[34]

Bhatia M R, Crook K A W. 1986. Trace element characteristics of graywackes and tectonic setting discrimination of sedimentary basins[J]. Contributions to Mineralogy and Petrology, 92(2): 181-193.

[35]

Burke W H, Denison R E, Hetherington E A, et al. 1982. Variation of seawater ⁸⁷Sr/⁸⁶Sr throughout Phanerozoic time[J]. Geology, 10(10): 516-519.

[36]

Douville E, Bienvenu P, Charlou J L, et al. 1999. Yttrium and rare earth elements in fluids from various deep-sea hydrothermal systems[J]. Geochimica et Cosmochimica Acta, 63(5): 627-643.

[37]

Frimmel H E. 2009. Trace element distribution in Neoproterozoic carbonates as palaeoenvironmental indicator[J]. Chemical Geology, 258(3/4): 338-353.

[38]

Gomes J M P, Rios-Netto A M, Borghi L, et al. 2021. Cyclostratigraphic analysis of the Early Cretaceous laminated limestones of the Araripe Basin, NE Brazil: Estimating sedimentary depositional rates[J]. Journal of South American Earth Sciences, 112: 103563.

[39]

Hallam A. 1986. Origin of minor limestone-shale cycles: Climatically induced or diagenetic?[J]. Geology, 14(7): 609-612.

[40]

Hu Z W, Huang S J, Li Z M, et al. 2013. Geochemical characteristics of the Permian Changxing Formation reef dolomites, northeastern Sichuan Basin, China[J]. Petroleum Science, 10(1): 38-49.

[41]

Kakuwa Y, Matsumoto R. 2006. Cerium negative anomaly just before the Permian and Triassic boundary event—the upward expansion of anoxia in the water column[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 229(4): 335-344.

[42]

Li J, Cai Z X, Chen H R, et al. 2018. Influence of differential diagenesis on primary depositional signals in limestone-marl alternations: An example from Middle Permian marine successions, South China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 495: 139-151.

[43]

Luan G Q, Azmy K, Berra F, et al. 2022. Origin of dolomites in oolitic carbonates of the Middle Jurassic Dorgali Formation, eastern Sardinia, Italy: Petrographic and geochemical constraints[J]. Marine and Petroleum Geology, 135: 105395.

[44]

Munnecke A, Westphal H. 2004. Shallow-water aragonite recorded in bundles of limestone-marl alternations-the Upper Jurassic of SW Germany[J]. Sedimentary Geology, 164(3/4): 191-202.

[45]

Pang Q, Hu G, Zhang X H, et al. 2021. Organic geochemistry, sedimentary environment, and organic matter enrichment of limestone-marlstone rhythms in the Middle Permian northern Sichuan Basin, China[J]. Marine and Petroleum Geology, 2021, 134: 105306.

[46]

Raiswell R. 1988. Chemical model for the origin of minor limestone-shale cycles by anaerobic methane oxidation[J]. Geology, 16(7): 641-644.

[47]

Shi J Y, Jin Z J, Liu Q Y, et al. 2021. Sunspot cycles recorded in Eocene lacustrine fine-grained sedimentary rocks in the Bohai Bay Basin, eastern China[J]. Global and Planetary Change, 205: 103614.

[48]

Vasconcelos C, Mckenzie J A. 1997. Microbial mediation of modern dolomite precipitation and diagenesis under anoxic conditions (Lagoa Vermelha, Rio de Janeiro, Brazil)[J]. Journal of Sedimentary Research, 67(3): 378-390.

[49]

Veizer J. 1983. Chemical diagenesis of carbonates: Theory and application of trace element technique[M]//Arthur M A, Anderson T F, Kaplan I R, et al. Stable isotopes in sedimentary geology. Tulsa: SEPM Society for Sedimentary Geology: 1-100.

[50]

Veizer J, Ala D, Azmy K, et al. 1999. ⁸⁷Sr/⁸⁶Sr, δ ¹³C and δ ¹⁸O evolution of Phanerozoic seawater[J]. Chemical Geology, 161(1/2/3): 59-88.

[51]

Warren J. 2000. Dolomite: Occurrence, evolution and economically important associations[J]. Earth-Science Reviews, 52(1/2/3): 1-81.

[52]

Westphal H. 2006. Limestone-marl alternations as environmental archives and the role of early diagenesis: A critical review[J]. International Journal of Earth Sciences, 95(6): 947-961.

[1]	陈武，季寿元. 1985. 矿物学导论[M]. 北京：地质出版社：1-297. Chen Wu, Ji Shouyuan. 1985. An introdluction to mineralogy[M]. Beijing: Geological Publishing House: 1-297.
[2]	陈轩，赵文智，张利萍，等. 2012. 川中地区中二叠统构造热液白云岩的发现及其勘探意义[J]. 石油学报，33（4）：562-569. Chen Xuan, Zhao Wenzhi, Zhang Liping, et al. 2012. Discovery and exploration significance of structure-controlled hydrothermal dolomites in the Middle Permian of the central Sichuan Basin[J]. Acta Petrolei Sinica, 33(4): 562-569.
[3]	冯增昭，王英华，刘焕杰，等. 1994. 中国沉积学[M]. 北京：石油工业出版社：1- 968. Feng Zengzhao, Wang Yinghua, Liu Huanjie, et al. 1994. Sedimentology of China[M]. Beijing: Petroleum Industry Press: 1-968.
[4]	韩月卿，郝运轻，韩文彪，等. 2022. 川东南地区中二叠统茅口组一段眼球状灰岩成因机理[J]. 油气地质与采收率，29（6）：12-21. Han Yueqing, Hao Yunqing, Han Wenbiao, et al. 2022. Genetic mechanism of eyeball-shaped limestone in First member of Middle Permian Maokou Formation in southeast Sichuan Basin[J]. Petroleum Geology and Recovery Efficiency, 29(6): 12-21.
[5]	何明薇，罗进雄. 2016. 湖北兴山峡口中二叠统眼球状石灰岩特征及成因[J]. 长江大学学报（自科版），13（14）：1-8. He Mingwei, Luo Jinxiong. 2016. Origin and characteristics of Middle Permian eyeball-shaped limestone in Xiakou area of Xingshan county of Hubei province[J]. Journal of Yangtze University (Natural Science Edition), 13(14): 1-8.
[6]	赫云兰，刘波，秦善. 2010. 白云石化机理与白云岩成因问题研究[J]. 北京大学学报（自然科学版），46（6）：1010-1020. He Yunlan, Liu Bo, Qin Shan. 2010. Study on the dolomitization and dolostone genesis[J]. Acta Scientiarum Naturalium Universitatis Pekinensis, 46(6): 1010-1020.
[7]	何溥为，胥旺，张连进，等. 2021. 川中磨溪—高石梯地区栖霞组白云岩特征及成因机制[J]. 沉积学报，39（6）：1532-1545. He Puwei, Xu Wang, Zhang Lianjin, et al. 2021. Characteristics and genetic mechanism of Qixia Formation dolomite in Moxi-Gaoshiti area, central Sichuan Basin[J]. Acta Sedimentologica Sinica, 39(6): 1532-1545.
[8]	胡东风，王良军，黄仁春，等. 2019. 四川盆地东部地区中二叠统茅口组白云岩储层特征及其主控因素[J]. 天然气工业，39（6）：13-21. Hu Dongfeng, Wang Liangjun, Huang Renchun, et al. 2019. Characteristics and main controlling factors of the Middle Permian Maokou dolomite reservoirs in the eastern Sichuan Basin[J]. Natural Gas Industry, 39(6): 13-21.
[9]	胡明毅，胡忠贵，魏国齐，等. 2012. 四川盆地茅口组层序岩相古地理特征及储集层预测[J]. 石油勘探与开发，39（1）：45-55. Hu Mingyi, Hu Zhonggui, Wei Guoqi, et al. 2012. Sequence lithofacies paleogeography and reservoir prediction of the Maokou Formation in Sichuan Basin[J]. Petroleum Exploration and Development, 39(1): 45-55.
[10]	胡文碹，陈琪，王小林，等. 2010. 白云岩储层形成演化过程中不同流体作用的稀土元素判别模式[J]. 石油与天然气地质，2010，31（6）：810-818. Hu Wenxuan, Chen Qi, Wang Xiaolin, et al. 2010. REE models for the discrimination of fluids in the formation and evolution of dolomite reservoirs[J]. Oil & Gas Geology, 31(6): 810-818.
[11]	黄思静. 1997. 上扬子地台区晚古生代海相碳酸盐岩的碳、锶同位素研究[J]. 地质学报，71（1）：45-53. Huang Sijing. 1997. A study on carbon and strontium isotopes of Late Paleozoic carbonate rocks in the Upper Yangtze Platform[J]. Acta Geologica Sinica, 71(1): 45-53.
[12]	黄思静，卿海若，胡作维，等. 2008. 川东三叠系飞仙关组碳酸盐岩的阴极发光特征与成岩作用[J]. 地球科学：中国地质大学学报，33（1）：26-34. Huang Sijing, Hairuo Qing, Hu Zuowei, et al. 2008. Cathodoluminescence and diagenesis of the carbonate rocks in Feixianguan Formation of Triassic, eastern Sichuan Basin of China[J]. Earth Science: Journal of China University of Geosciences, 33(1): 26-34.
[13]	李大军，陈辉，陈洪德，等. 2016. 四川盆地中二叠统茅口组储层形成与古构造演化关系[J]. 石油与天然气地质，37（5）：756-763. Li Dajun, Chen Hui, Chen Hongde, et al. 2016. Relationship between reservoir development in the Middle Permian Maokou Formation and paleostructure evolution in the Sichuan Basin[J]. Oil & Gas Geology, 37(5): 756-763.
[14]	梁兴，徐政语，栗维民，等. 2023. 蜀南—渝西地区中二叠统茅一段灰质源岩气储层特征及主控因素：以DB1井为例[J]. 石油实验地质，45（4）：714-725. Liang Xing, Xu Zhengyu, Li Weimin, et al. 2023. Characteristics and main controlling factors of the limy source rock gas reservoir in the First member of the Middle Permian Maokou Formation in the southern Sichuan and western Chongqing area: A case study of well DB 1[J]. Petroleum Geology & Experiment, 45(4): 714-725.
[15]	刘瑾，夏文谦，李晶晶，等. 2019. 川东南地区茅一段储层特征分析[J]. 科技通报，35（7）：26-32. Liu Jin, Xia Wenqian, Li Jingjing, et al. 2019. Analysis of reservoir characteristics of the First member of Maokou Formation in southeastern Sichuan Basin[J]. Bulletin of Science and Technology, 35(7): 26-32.
[16]	刘喜停，颜佳新，马志鑫，等. 2014. 华南栖霞组灰岩—泥灰岩韵律层的成因[J]. 地球科学：中国地质大学学报，39（2）：155-164. Liu Xiting, Yan Jiaxin, Ma Zhixin, et al. 2014. Origination of limestone-marl alternations from Qixia Formation of South China[J]. Earth Science: Journal of China University of Geosciences, 39(2): 155-164.
[17]	罗进雄，何幼斌. 2010. 中—上扬子地区二叠系眼球状石灰岩特征及成因研究[J]. 地质论评，56（5）：629-637. Luo Jinxiong, He Youbin. 2010. Origin and characteristics of Permian eyeball-shaped limestones in Middle-Upper Yangtze region[J]. Geological Review, 56(5): 629-637.
[18]	罗进雄，何幼斌. 2014. 中上扬子地区二叠系烃源岩特征[J]. 天然气地球科学，25（9）：1416-1425. Luo Jinxiong, He Youbin. 2014. Characteristics of the Permian source rocks in the Middle and Upper Yangtze region[J]. Natural Gas Geoscience, 5(9): 1416-1425.
[19]	罗进雄，何幼斌，何明薇，等. 2019. 华南中二叠统眼球状石灰岩特征及成因的思考[J]. 古地理学报，21（4）：613-626. Luo Jinxiong, He Youbin, He Mingwei, et al. 2019. Thoughts on characteristics and origin of the Middle Permian eyeball-shaped limestone in South China[J]. Journal of Palaeogeography, 21(4): 613-626.
[20]	任海侠，林小兵，刘叶，等. 2021. 川西南二叠系茅口组一段滑石特征及其形成机理：以A1井茅一段样品为例[J]. 石油实验地质，43（6）：1038-1047. Ren Haixia, Lin Xiaobing, Liu Ye, et al. 2021. Characteristics and formation mechanism of talc in Permian Maokou Formation, southwestern Sichuan Basin: A case study of First member of Maokou Formation in well A1[J]. Petroleum Geology & Experiment, 43(6): 1038-1047.
[21]	任梦怡，江青春，汪泽成，等. 2020. 川南地区中二叠统茅口组成岩流体来源及演化过程[J]. 天然气工业，40（4）：40-50. Ren Mengyi, Jiang Qingchun, Wang Zecheng, et al. 2020. Source and evolution of diagenetic fluid in the Middle Permian Maokou Formation in the southern Sichuan Basin[J]. Natural Gas Industry, 40(4): 40-50.
[22]	宋翠玉，吕大炜. 2022. 米兰科维奇旋回时间序列分析法研究进展[J]. 沉积学报，40（2）：380-395. Song Cuiyu, Dawei Lü. 2022. Advances in time series analysis methods for Milankovitch cycles[J]. Acta Sedimentologica Sinica, 40(2): 380-395.
[23]	唐雨，张云峰，胡林辉，等. 2021. 开江—梁平海槽西侧中东段长兴组台缘储层特征及差异性[J]. 沉积学报，2021，39（6）：1593-1608. Tang Yu, Zhang Yunfeng, Hu Linhui, et al. 2021. Characteristics and differences of the platform margin reservoir, Changxing Formation, central eastern region, west of the Kaijiang-Liangping trough[J]. Acta Sedimentologica Sinica, 39(6): 1593-1608.
[24]	王良军，李红，曾韬，等. 2022. 四川盆地东部茅口组白云岩成因：来自岩石学、矿物学和地球化学的证据[J]. 古地理学报，24（5）：989-1016. Wang Liangjun, Li Hong, Zeng Tao, et al. 2022. Origins of dolostones of the Maokou Formation in eastern Sichuan Basin: Evidence from lithology, mineralogy, and geochemistry[J]. Journal of Palaeogeography, 24(5): 989-1016.
[25]	向娟，胡明毅，胡忠贵，等. 2011.四川盆地中二叠统茅口组沉积相分析[J]. 石油地质与工程，25（1）：14-19. Xiang Juan, Hu Mingyi, Hu Zhonggui, et al. 2011.Sedimentary facies analysis of Maokou Formation of Middle Permian in Sichuan Basin[J]. Petroleum Geology and Engineering, 25(1): 14-19.
[26]	许国明，谢刚平，隆轲，等. 2015. 四川盆地西南部中二叠统沉积特征与勘探目标[J]. 天然气工业，35（7）：27-33. Xu Guoming, Xie Gangping, Long Ke, et al. 2015. Sedimentary features and exploration targets of Middle Permian reservoirs in the southwestern Sichuan Basin[J]. Natural Gas Industry, 35(7): 27-33.
[27]	薛武强，刘喜停，颜佳新，等. 2015. 重庆南川地区中二叠统茅口组眼球状灰岩成因[J]. 地质科学，50（3）：1001-1013. Xue Wuqiang, Liu Xiting, Yan Jiaxin, et al. 2015. The origin of eyeball-shaped limestone from Maokou Formation (Mid-Permian) in Nanchuan region, Chongqing, Southwest China[J]. Chinese Journal of Geology, 50(3): 1001-1013.
[28]	于春勇，崔军平，王起琮，等. 2020. 鄂尔多斯盆地南部奥陶系马家沟组中下组合白云岩稀土元素特征及其成因[J]. 西北大学学报（自然科学版），50（5）：819-830. Yu Chunyong, Cui Junping, Wang Qicong, et al. 2020. The REE characteristics and genesis of the middle and lower combinations dolomite of Ordovician Majiagou in the southern Ordos Basin[J]. Journal of Northwest University (Natural Science Edition), 50(5): 819-830.
[29]	张宝民，单秀琴，张静，等. 2017. 中国海相碳酸盐岩储层地质与成因[M]. 北京：科学出版社：1- 617. Zhang Baomin, Shan Xiuqin, Zhang Jing, et al. 2017. Geology and genesis of marine carbonate reservoirs in China[M]. Beijing: Science Press: 1-617.
[30]	张涛，苏玉山，佘刚，等. 2015. 热液白云岩发育模式：以扎格罗斯盆地白垩系A油田为例[J]. 石油与天然气地质，36（3）：393-401. Zhang Tao, Su Yushan, She Gang, et al. 2015. A study on the genetic model of hydrothermal dolomitization in Taq Taq oilfield, Kurdistan region, Iraq—taking oilfield A in the Cretaceous in Zagros Basin as an example[J]. Oil & Gas Geology, 36(3): 393-401.
[31]	张玺华，陈聪，黄婕，等. 2019. 四川盆地中二叠世广元—巴中拉张槽的发现及其油气地质意义[J]. 中国石油勘探，24（4）：466-475. Zhang Xihua, Chen Cong, Huang Jie, et al. 2019. The discovery of Middle Permian Guangyuan-Bazhong extensional trough in the Sichuan Basin and its petroleum geological significance[J]. China Petroleum Exploration, 24(4): 466-475.
[32]	张玺华，陈聪，张亚，等. 2018. 川西北地区茅口组海槽相地质特征及其油气地质意义[J]. 天然气勘探与开发，41（3）：42-50. Zhang Xihua, Chen Cong, Zhang Ya, et al. 2018. Geological characteristics of trough facies, Maokou Formation, northwestern Sichuan Basin: Implications for geology[J]. Natural Gas Exploration and Development, 41(3): 42-50.
[33]	Bau M. 1996. Controls on the fractionation of isovalent trace elements in magmatic and aqueous systems: Evidence from Y/Ho, Zr/Hf, and lanthanide tetrad effect[J]. Contributions to Mineralogy and Petrology, 123(3): 323-333.
[34]	Bhatia M R, Crook K A W. 1986. Trace element characteristics of graywackes and tectonic setting discrimination of sedimentary basins[J]. Contributions to Mineralogy and Petrology, 92(2): 181-193.
[35]	Burke W H, Denison R E, Hetherington E A, et al. 1982. Variation of seawater ⁸⁷Sr/⁸⁶Sr throughout Phanerozoic time[J]. Geology, 10(10): 516-519.
[36]	Douville E, Bienvenu P, Charlou J L, et al. 1999. Yttrium and rare earth elements in fluids from various deep-sea hydrothermal systems[J]. Geochimica et Cosmochimica Acta, 63(5): 627-643.
[37]	Frimmel H E. 2009. Trace element distribution in Neoproterozoic carbonates as palaeoenvironmental indicator[J]. Chemical Geology, 258(3/4): 338-353.
[38]	Gomes J M P, Rios-Netto A M, Borghi L, et al. 2021. Cyclostratigraphic analysis of the Early Cretaceous laminated limestones of the Araripe Basin, NE Brazil: Estimating sedimentary depositional rates[J]. Journal of South American Earth Sciences, 112: 103563.
[39]	Hallam A. 1986. Origin of minor limestone-shale cycles: Climatically induced or diagenetic?[J]. Geology, 14(7): 609-612.
[40]	Hu Z W, Huang S J, Li Z M, et al. 2013. Geochemical characteristics of the Permian Changxing Formation reef dolomites, northeastern Sichuan Basin, China[J]. Petroleum Science, 10(1): 38-49.
[41]	Kakuwa Y, Matsumoto R. 2006. Cerium negative anomaly just before the Permian and Triassic boundary event—the upward expansion of anoxia in the water column[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 229(4): 335-344.
[42]	Li J, Cai Z X, Chen H R, et al. 2018. Influence of differential diagenesis on primary depositional signals in limestone-marl alternations: An example from Middle Permian marine successions, South China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 495: 139-151.
[43]	Luan G Q, Azmy K, Berra F, et al. 2022. Origin of dolomites in oolitic carbonates of the Middle Jurassic Dorgali Formation, eastern Sardinia, Italy: Petrographic and geochemical constraints[J]. Marine and Petroleum Geology, 135: 105395.
[44]	Munnecke A, Westphal H. 2004. Shallow-water aragonite recorded in bundles of limestone-marl alternations-the Upper Jurassic of SW Germany[J]. Sedimentary Geology, 164(3/4): 191-202.
[45]	Pang Q, Hu G, Zhang X H, et al. 2021. Organic geochemistry, sedimentary environment, and organic matter enrichment of limestone-marlstone rhythms in the Middle Permian northern Sichuan Basin, China[J]. Marine and Petroleum Geology, 2021, 134: 105306.
[46]	Raiswell R. 1988. Chemical model for the origin of minor limestone-shale cycles by anaerobic methane oxidation[J]. Geology, 16(7): 641-644.
[47]	Shi J Y, Jin Z J, Liu Q Y, et al. 2021. Sunspot cycles recorded in Eocene lacustrine fine-grained sedimentary rocks in the Bohai Bay Basin, eastern China[J]. Global and Planetary Change, 205: 103614.
[48]	Vasconcelos C, Mckenzie J A. 1997. Microbial mediation of modern dolomite precipitation and diagenesis under anoxic conditions (Lagoa Vermelha, Rio de Janeiro, Brazil)[J]. Journal of Sedimentary Research, 67(3): 378-390.
[49]	Veizer J. 1983. Chemical diagenesis of carbonates: Theory and application of trace element technique[M]//Arthur M A, Anderson T F, Kaplan I R, et al. Stable isotopes in sedimentary geology. Tulsa: SEPM Society for Sedimentary Geology: 1-100.
[50]	Veizer J, Ala D, Azmy K, et al. 1999. ⁸⁷Sr/⁸⁶Sr, δ ¹³C and δ ¹⁸O evolution of Phanerozoic seawater[J]. Chemical Geology, 161(1/2/3): 59-88.
[51]	Warren J. 2000. Dolomite: Occurrence, evolution and economically important associations[J]. Earth-Science Reviews, 52(1/2/3): 1-81.
[52]	Westphal H. 2006. Limestone-marl alternations as environmental archives and the role of early diagenesis: A critical review[J]. International Journal of Earth Sciences, 95(6): 947-961.