[1] Hardie L A. Dolomitization: A critical view of some current views[J]. Journal of Sedimentary Petrology, 1987, 57(1): 166-183.
[2] Machel H G. Concepts and models of dolomitization: A critical reappraisal[J]. Geological Society, London, Special Publications, 2004, 235: 7-63.
[3] Warren J. Dolomite: Occurrence, evolution and economically important associations[J]. Earth-Science Reviews, 2000, 52(1/2/3): 1-81.
[4] Zenger D H, Dunham J B, Ethington R L. Concepts and models of dolomitization[M]. Tulsa: SEPM Society for Sedimentary Geology, 1980: 320.
[5] 何治亮,马永生,张军涛,等. 中国的白云岩与白云岩储层:分布、成因与控制因素[J]. 石油与天然气地质,2020,41(1):1-14.

He Zhiliang, Ma Yongsheng, Zhang Juntao, et al. Distribution, genetic mechanism and control factors of dolomite and dolomite reservoirs in China[J]. Oil & Gas Geology, 2020, 41(1): 1-14.
[6] 金之钧. 中国海相碳酸盐岩层系油气形成与富集规律[J]. 中国科学(D辑):地球科学,2011,41(7):910-926.

Jin Zhijun. Formation and accumulation of oil and gas in marine carbonate strata in Chinese sedimentary basins[J]. Science China (Seri.D): Earth Sciences, 2011, 41(7): 910-926.
[7] 陈代钊,钱一雄. 深层—超深层白云岩储集层:机遇与挑战[J]. 古地理学报,2017,19(2):187-196.

Chen Daizhao, Qian Yixiong. Deep or super-deep dolostone reservoirs: Opportunities and challenges[J]. Journal of Palaeogeography, 2017, 19(2): 187-196.
[8] 尤东华,韩俊,胡文瑄,等. 塔里木盆地顺南501井鹰山组白云岩储层特征与成因[J]. 沉积学报,2018,36(6):1206-1217.

You Donghua, Han Jun, Hu Wenxuan, et al. Characteristics and genesis of dolomite reservoirs in the Yingshan Formation of well SN501 in the Tarim Basin[J]. Acta Sedimentologica Sinica, 2018, 36(6): 1206-1217.
[9] 郑剑锋,沈安江,乔占峰,等. 柯坪—巴楚露头区蓬莱坝组白云岩特征及孔隙成因[J]. 石油学报,2014,35(4):664-672.

Zheng Jianfeng, Shen Anjiang, Qiao Zhanfeng, et al. Characteristics and pore genesis of dolomite in the Penglaiba Formation in Keping-Bachu outcrop area[J]. Acta Petrolei Sinica, 2014, 35(4): 664-672.
[10] 乔占峰,沈安江,郑剑锋,等. 塔里木盆地下奥陶统白云岩类型及其成因[J]. 古地理学报,2012,14(1):21-32.

Qiao Zhanfeng, Shen Anjiang, Zheng Jianfeng, et al. Classification and origin of the Lower Ordovician dolostone in Tarim Basin[J]. Journal of Palaeogeography, 2012, 14(1): 21-32.
[11] Guo C, Chen D Z, Qing H R, et al. Early dolomitization and recrystallization of the Lower-Middle Ordovician carbonates in western Tarim Basin (NW China)[J]. Marine and Petroleum Geology, 2020, 111: 332-349.
[12] Guo C, Chen D Z, Qing H R, et al. Multiple dolomitization and later hydrothermal alteration on the Upper Cambrian-Lower Ordovician carbonates in the northern Tarim Basin, China[J]. Marine and Petroleum Geology, 2016, 72: 295-316.
[13] 邵龙义,何宏,彭苏萍,等. 塔里木盆地巴楚隆起寒武系及奥陶系白云岩类型及形成机理[J]. 古地理学报,2002,4(2):19-30.

Shao Longyi, He Hong, Peng Suping, et al. Types and origin of dolostones of the Cambrian and Ordovician of Bachu uplift area in Tarim Basin[J]. Journal of Palaeogeography, 2002, 4(2): 19-30.
[14] 乔占峰,张天付,贺训云,等. 塔里木盆地蓬莱坝组层状白云岩储层发育规律[J]. 地球科学,2023,48(2):673-689.

Qiao Zhanfeng, Zhang Tianfu, He Xunyun, et al. Development and exploration direction of bedded massive dolomite reservoir of Lower Ordovician Penglaiba Formation in Tarim Basin[J]. Earth Science, 2023, 48(2): 673-689.
[15] 曹自成,尤东华,漆立新,等. 塔里木盆地塔深1井超深层白云岩储层成因新认识:来自原位碳氧同位素分析的证据[J]. 天然气地球科学,2020,31(7):915-922.

Cao Zicheng, You Donghua, Qi Lixin, et al. New insights of the genesis of ultra-deep dolomite reservoirs in well TS1, Tarim Basin: Evidence from in situ carbon and oxygen isotope analysis[J]. Natural Gas Geoscience, 2020, 31(7): 915-922.
[16] 王丹,王旭,陈代钊,等. 塔里木盆地塔北、塔中地区寒武系—奥陶系碳酸盐岩中鞍形白云石胶结物特征[J]. 地质科学,2010,45(2):580-594.

Wang Dan, Wang Xu, Chen Daizhao, et al. Characteristics of saddle dolomite cements in the Cambrian-Ordovician carbonates in Tabei and Tazhong area of Tarim Basin[J]. Chinese Journal of Geology, 2010, 45(2): 580-594.
[17] 郑和荣,吴茂炳,邬兴威,等. 塔里木盆地下古生界白云岩储层油气勘探前景[J]. 石油学报,2007,28(2):1-8.

Zheng Herong, Wu Maobing, Wu Xingwei, et al. Oil-gas exploration prospect of dolomite reservoir in the Lower Paleozoic of Tarim Basin[J]. Acta Petrolei Sinica, 2007, 28(2): 1-8.
[18] Zhu D Y, Meng Q Q, Jin Z J, et al. Formation mechanism of deep Cambrian dolomite reservoirs in the Tarim Basin, northwestern China[J]. Marine and Petroleum Geology, 2015, 59: 232-244.
[19] 漆立新. 塔里木盆地顺托果勒隆起奥陶系碳酸盐岩超深层油气突破及其意义[J]. 中国石油勘探,2016,21(3):38-51.

Qi Lixin. Oil and gas breakthrough in ultra-deep Ordovician carbonate formations in Shuntuoguole uplift, Tarim Basin[J]. China Petroleum Exploration, 2016, 21(3): 38-51.
[20] 顾家裕. 塔里木盆地下奥陶统白云岩特征及成因[J]. 新疆石油地质,2000,21(2):120-122,170.

Gu Jiayu. Characteristics and origin analysis of dolomite in Lower Ordovician of Tarim Basin[J]. Xinjiang Petroleum Geology, 2000, 21(2): 120-122, 170.
[21] 郭峰,郭岭. 柯坪地区肖尔布拉克寒武系层序及沉积演化[J]. 地层学杂志,2011,35(2):164-171.

Guo Feng, Guo Ling. Sequence stratigraphy and sedimentary evolution of the Cambrian system at the Xiaoerblak section in the Keping area[J]. Journal of Stratigraphy, 2011, 35(2): 164-171.
[22] 赵宗举,张运波,潘懋,等. 塔里木盆地寒武系层序地层格架[J]. 地质论评,2010,56(5):609-620.

Zhao Zongju, Zhang Yunbo, Pan Mao, et al. Cambrian sequence stratigraphic framework in Tarim Basin[J]. Geological Review, 2010, 56(5): 609-620.
[23] McLennan S M. Rare earth elements in sedimentary rocks: Influence of provenance and sedimentary processes[J]. Reviews in Mineralogy and Geochemistry, 1989, 21(1): 169-200.
[24] Gregg J M, Sibley D F. Epigenetic dolomitization and the origin of xenotopic dolomite texture[J]. Journal of Sedimentary Petrology, 1984, 54(3): 908-931.
[25] Sibley D F, Gregg J M. Classification of dolomite rock textures[J]. Journal of Sedimentary Petrology, 1987, 57(6): 967-975.
[26] 王丹,陈代钊,杨长春,等. 埋藏环境白云石结构类型[J]. 沉积学报,2010,28(1):17-25.

Wang Dan, Chen Daizhao, Yang Changchun, et al. Classification of texture in burial dolomite[J]. Acta Sedimentologica Sinica, 2010, 28(1): 17-25.
[27] Lind I L. Stylolites in chalk from Leg 130, Ontong Java Plateau[J]. Proceedings of the Ocean Drilling Program, Scientific Results, 1993, 130: 445-451.
[28] Fabricius I L, Borre M K. Stylolites, porosity, depositional texture, and silicates in chalk facies sediments. Ontong Java Plateau-Gorm and Tyra fields, North Sea[J]. Sedimentology, 2007, 54(1): 183-205.
[29] Qing H R, Mountjoy E W. Formation of coarsely crystalline, hydrothermal dolomite reservoirs in the Presqu'ile barrier, western Canada sedimentary basin[J]. AAPG Bulletin, 1994, 78(1): 55-77.
[30] Chen D Z, Qing H R, Yang C. Multistage hydrothermal dolomites in the Middle Devonian (Givetian) carbonates from the Guilin area, South China[J]. Sedimentology, 2004, 51(5): 1029-1051.
[31] Tucker M E, Wright V P. Carbonate sedimentology[M]. Oxford: Blackwell Science, 1990: 1-482.
[32] 陈永权,周新源. 塔里木盆地中寒武统—下奥陶统泥晶灰岩地球化学与古海洋学[J]. 海洋地质与第四纪地质,2009,29(1):47-52.

Chen Yongquan, Zhou Xinyuan. Geochemical characteristics of Middle Cambrian-Early Ordovician limestone and paleo-ocean reconstruction based on δ18OSMOW, 87Sr/86Sr and rare earth elements, Tarim Basin[J]. Marine Geology & Quaternary Geology, 2009, 29(1): 47-52.
[33] 陈永权,周新源,赵葵东,等. 塔里木盆地塔中19井奥陶系蓬莱坝组云灰互层段的岩性旋回特征与“顶侵型”埋藏云化模式的建立[J]. 沉积学报,2009,27(2):202-211.

Chen Yongquan, Zhou Xinyuan, Zhao Kuidong, et al. The petrologic rhythm of Lower Ordovician Penglaiba Formation encountered by well Tazhong 19 and new dolomitization model, Tarim Basin[J]. Acta Sedimentologica Sinica, 2009, 27(2): 202-211.
[34] 朱东亚,金之钧,胡文瑄. 塔北地区下奥陶统白云岩热液重结晶作用及其油气储集意义[J]. 中国科学(D辑):地球科学,2010,40(2):156-170.

Zhu Dongya, Jin Zhijun, Hu Wenxuan. Hydrothermal recrystallization of the Lower Ordovician dolomite and its significance to reservoir in northern Tarim Basin[J]. Science China (Seri.D): Earth Sciences, 2010, 40(2): 156-170.
[35] Fan R, Deng S H, Zhang X L. Significant carbon isotope excursions in the Cambrian and their implications for global correlations[J]. Science China Earth Sciences, 2011, 54(11): 1686-1695.
[36] Veizer J, Ala D, Azmy K, et al. 87Sr/86Sr, δ13C and δ18O evolution of Phanerozoic seawater[J]. Chemical Geology, 1999, 161: 59-88.
[37] Montañez I P, Osleger D A, Banner J L, et al. Evolution of the Sr and C isotope composition of Cambrian oceans[J]. GSA Today, 2000, 10(5): 1-7.
[38] Zhao Y Y, Zheng Y F, Chen F K. Trace element and strontium isotope constraints on sedimentary environment of Ediacaran carbonates in southern Anhui, South China[J]. Chemical Geology, 2009, 265(3/4): 345-362.
[39] Zhao Y Y, Wei W, Li S Z, et al. Rare earth element geochemistry of carbonates as a proxy for deep-time environmental reconstruction[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2021, 574: 110443.
[40] Zhao Y Y, Wei W, Santosh M, et al. A review of retrieving pristine rare earth element signatures from carbonates[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2022, 586: 110765.
[41] Ward J F, Verdel C, Campbell M J, et al. Rare earth element geochemistry of Australian Neoproterozoic carbonate: Constraints on the Neoproterozoic oxygenation events[J]. Precambrian Research, 2019, 335: 105471.
[42] Morad S, Felitsyn S. Identification of primary Ce-anomaly signatures in fossil biogenic apatite: Implication for the Cambrian oceanic anoxia and phosphogenesis[J]. Sedimentary Geology, 2001, 143(3/4): 259-264.
[43] Shields G, Stille P. Diagenetic constraints on the use of cerium anomalies as palaeoseawater redox proxies: An isotopic and REE study of Cambrian phosphorites[J]. Chemical Geology, 2001, 175(1/2): 29-48.
[44] Mazzullo S J. Organogenic dolomitization in peritidal to deep-sea sediments[J]. Journal of Sedimentary Research, 2000, 70(1): 10-23.
[45] McKenzie J A. Holocene dolomitization of calcium carbonate sediments from the coastal sabkhas of Abu Dhabi, U.A.E.: A stable isotope study[J]. The Journal of Geology, 1981, 89(2): 185-198.
[46] Webb G E, Kamber B S. Rare earth elements in Holocene reefal microbialites: A new shallow seawater proxy[J]. Geochimica et Cosmochimica Acta, 2000, 64(9): 1557-1565.
[47] Wang G W, Hao F, Li P P, et al. Use of rare earth element geochemistry to constrain the source of dolomitizing fluid for dolomitization of the Lower Triassic Feixianguan Formation, Jiannan area, China[J]. Journal of Petroleum Science and Engineering, 2016, 138: 282-291.
[48] Scotese C R, McKerrow W S. Revised world maps and introduction[M]//McKerrow W S, Scotese C R. Paleozoic paleogeography and biogeography. London: Geological Society, London, Memoirs, 1990, 12: 1-21.
[49] Wright D T. The role of sulphate-reducing bacteria and cyanobacteria in dolomite formation in distal ephemeral lakes of the Coorong region, South Australia[J]. Sedimentary Geology, 1999, 126: 147-157.
[50] Jiang L, Cai C F, Worden R H, et al. Multiphase dolomitization of deeply buried Cambrian petroleum reservoirs, Tarim Basin, north-west China[J]. Sedimentology, 2016, 63(7): 2130-2157.
[51] Qing H R, Bosence D W J, Rose E P F. Dolomitization by penesaline sea water in Early Jurassic peritidal platform carbonates, Gibraltar, western Mediterranean[J]. Sedimentology, 2001, 48(1): 153-163.
[52] Vasconcelos C, McKenzie J A. Microbial mediation of modern dolomite precipitation and diagenesis under anoxic conditions (Lagoa Vermelha, Rio de Janeiro, Brazil)[J]. Journal of Sedimentary Research, 1997, 67(3): 378-390.
[53] van Lith Y, Warthmann R, Vasconcelos C, et al. Sulphate-reducing bacteria induce low-temperature Ca-dolomite and high Mg-calcite formation[J]. Geobiology, 2003, 1(1): 71-79.
[54] Guo C, Chen D Z, Dong S F, et al. Early dolomitisation of the Lower-Middle Ordovician cyclic carbonates in northern Tarim Basin, NW China[J]. Science China Earth Sciences, 2017, 60(7): 1283-1298.
[55] Adams J E, Rhodes M L. Dolomitization by seepage refluxion[J]. AAPG Bulletin, 1960, 44(12): 1912-1920.
[56] You X L, Sun S, Zhu J Q, et al. Microbially mediated dolomite in Cambrian stromatolites from the Tarim Basin, north-west China: Implications for the role of organic substrate on dolomite precipitation[J]. Terra Nova, 2013, 25(5): 387-395.
[57] 胡文瑄,朱井泉,王小林,等. 塔里木盆地柯坪地区寒武系微生物白云岩特征、成因及意义[J]. 石油与天然气地质,2014,35(6):860-869.

Hu Wenxuan, Zhu Jingquan, Wang Xiaolin, et al. Characteristics, origin and geological implications of the Cambrian microbial dolomite in Keping area, Tarim Basin[J]. Oil & Gas Geology, 2014, 35(6): 860-869.
[58] Dong S F, Chen D Z, Qing H, et al. Hydrothermal alteration of dolostones in the Lower Ordovician, Tarim Basin, NW China: Multiple constraints from petrology, isotope geochemistry and fluid inclusion microthermometry[J]. Marine and Petroleum Geology, 2013, 46: 270-286.
[59] 李慧莉,邱楠生,金之钧,等. 塔里木盆地的热史[J]. 石油与天然气地质,2005,26(5):613-617.

Li Huili, Qiu Nansheng, Jin Zhijun, et al. Geothermal history of Tarim Basin[J]. Oil & Gas Geology, 2005, 26(5): 613-617.
[60] 邱楠生,汪集暘,梅庆华,等. (U-Th)/He年龄约束下的塔里木盆地早古生代构造—热演化[J]. 中国科学D辑:地球科学,2010,40(12):1669-1683.

Qiu Nansheng, Wang Jiyang, Mei Qinghua, et al. Constraints of (U-Th)/He ages on Early Paleozoic tectonothermal evolution of the Tarim Basin, China[J]. Science China: Earth Sciences, 2010, 40(12):1669-1683.
[61] Li K, Cai C, He H, et al. Origin of palaeo-waters in the Ordovician carbonates in Tahe oilfield, Tarim Basin: Constraints from fluid inclusions and Sr, C and O isotopes[J]. Geofluids, 2011, 11(1): 71-86.
[62] 傅强,凌支虎. 塔里木雅克拉断凸沉积埋藏史及成藏模式[J]. 成都理工学院学报,1996,23(2):74-79.

Fu Qiang, Ling Zhihu. The depositional history and the pool-forming models in the Yakela convex block, Tarim Basin[J]. Journal of Chengdu Institute of Technology, 1996, 23(2): 74-79.
[63] 叶德胜. 塔里木盆地北部寒武—奥陶系碳酸盐岩的深部溶蚀作用[J]. 沉积学报,1994,12(1):66-71.

Ye Desheng. Deep dissolution of Cambrian-Ordovician carbonates in the northern Tarim Basin[J]. Acta Sedimentologica Sinica, 1994, 12(1): 66-71.
[64] Qiu N S, Chang J, Zuo Y H, et al. Thermal evolution and maturation of Lower Paleozoic source rocks in the Tarim Basin, northwest China[J]. AAPG Bulletin, 2012, 96(5): 789-821.
[65] 黄思静. 碳酸盐岩的成岩作用[M]. 北京:地质出版社,2010.

Huang Sijing. Carbonate diagenesis[M]. Beijing: Geological Publishing House, 2010.
[66] Mattes B W, Mountjoy E W. Burial dolomitization of the Upper Devonian Miette buildup, Jasper National Park, Alberta[M]//Zenger D H, Dunham J B, Ethington R L. Concepts and models of dolomitization. Tulsa: SEPM Society for Sedimentary Geology, 1980: 259-297.
[67] 卿海若,陈代钊. 非热液成因的鞍形白云石:来自加拿大萨斯喀彻温省东南部奥陶系Yeoman组的岩石学和地球化学证据[J]. 沉积学报,2010,28(5):980-986.

Hairuo Qing, Chen Daizhao. Non-hydrothermal saddle dolomite: Petrological and geochemical evidence from the Ordovician Yeoman Formation, southeastern Saskatchewan, Canada[J]. Acta Sedimentologica Sinica, 2010, 28(5): 980-986.
[68] Dong S F, Chen D Z, Zhou X Q, et al. Tectonically driven dolomitization of Cambrian to Lower Ordovician carbonates of the Quruqtagh area, north-eastern flank of Tarim Basin, north-west China[J]. Sedimentology, 2017, 64(4): 1079-1106.