[1] BURCHETTE T P, WRIGHT V P.Carbonate ramp depositional systems[J]. Sedimentary Geology, 1992, 79(1/4): 3-57.
[2] MICHEL J, LAUGIÉ M, POHL A, et al.Marine carbonate factories: A global model of carbonate platform distribution[J]. International Journal of Earth Sciences, 2019, 108(6): 1773-1792.
[3] 金振奎, 石良, 高白水, 等. 碳酸盐岩沉积相及相模式[J]. 沉积学报, 2013, 31(6): 965-979.
JIN Zhenkui, SHI Liang, GAO Baishui, et al.Carbonate facies and facies models[J]. Acta Sedimentologica Sinica, 2013, 31(6): 965-979.
[4] CHEN J Q, PANG X Q, CHEN D X.Sedimentary facies and lithologic characters as main factors controlling hydrocarbon accumulations and their critical conditions[J]. Journal of Palaeogeography, 2015, 4(4): 413-429.
[5] 周刚, 钱红杉, 龙虹宇, 等. 上扬子区北缘宝塔组龟裂纹灰岩结构分异特征及发育模式[J]. 天然气勘探与开发, 2022, 45(3): 11-23.
ZHOU Gang, QIAN Hongsha, LONG Hongyu, et al.Structural differentiation and development model of cracked limestone of Pagoda Formation in northern margin of Upper Yangtze Region[J]. Natural Gas Exploration and Development, 2022, 45(3): 11-23.
[6] ZHANG Z H, PENG J, YANG G, et al.Characterization of sedimentary microfacies and depositional dynamics of the upper Cretaceous Hartha Formation in the X oil field, Middle East[J]. Carbonates and Evaporites, 2025, 40(2): 40.
[7] ZHANG Y F, TAN F, SUN Y B, et al.Differences between reservoirs in the intra-platform and platform margin reef-shoal complexes of the Upper Ordovician Lianglitag Formation in the Tazhong oil field, NW China, and corresponding exploration strategies[J]. Marine and Petroleum Geology, 2018, 98: 66-78.
[8] 王龙, 吴海, 张瑞, 等. 碳酸盐台地的类型、特征和沉积模式: 兼论华北地台寒武纪陆表海—淹没台地的沉积样式[J]. 地质论评, 2018, 64(1): 62-76.
WANG Long, WU Hai, ZHANG Rui, et al.The types, characteristics and depositional models of carbonate platform: Implications for Cambrian sedimentary patterns of epeiric-drowned carbonate platform in North China[J]. Geological Review, 2018, 64(1): 62-76.
[9] 朱长见, 肖中尧, 张宝民, 等. 塔里木盆地古城4井区上寒武统一奥陶系储集层特征[J]. 石油勘探与开发, 2008, 35(2): 175-181.
ZHU Changjian, XIAO Zhongyao, ZHANG Baomin, et al.Upper Cambrian-Ordovician reservoir characteristics in Well Gucheng-4 area, Tarim Basin[J]. Petroleum Exploration and Development, 2008, 35(2): 175-181.
[10] 吴光宏, 黎兵, 周新科, 等. 塔中古城墟隆起奥陶系钻探成果与勘探意义[J]. 新疆石油地质, 2007, 28(2): 154-157.
WU Guanghong, LI Bing, ZHOU Xinke, et al.The drilling efforts and significance of Ordovician in Guchengxu Uplift of Tazhong area[J]. Xinjiang Petroleum Geology, 2007, 28(2): 154-157.
[11] 刘艺妮, 胡明毅, 张三. 塔里木盆地古城—肖塘地区寒武系—奥陶系碳酸盐台地类型、差异演化过程及油气地质意义[J]. 石油勘探与开发, 2022, 49(5): 884-895.
LIU Yini, HU Mingyi, ZHANG San.Types, structural evolution difference and petroleum geological significance of Cambrian- Ordovician carbonate platforms in Gucheng-Xiaotang area, Tarim Basin, NW China[J]. Petroleum Exploration and Development, 2022, 49(5): 884-895.
[12] 刘艺妮, 胡明毅, 张三, 等. 碳酸盐缓坡沉积微相特征及其对储集层发育的制约: 以塔里木盆地古城地区中—下奥陶统为例[J]. 石油勘探与开发, 2022, 49(1): 93-105.
LIU Yini, HU Mingyi, ZHANG San, et al.Characteristics and impacts on favorable reservoirs of carbonate ramp microfacies: A case study of the Middle-Lower Ordovician in Gucheng area, Tarim Basin, NW China[J]. Petroleum Exploration and Development, 2022, 49(1): 93-105.
[13] 沈安江, 张友, 冯子辉, 等. 塔东古城地区碳酸盐岩储层地质认识与勘探领域[J]. 中国石油勘探, 2020, 25(3): 96-106.
SHEN Anjiang, ZHANG You, FENG Zihui, et al.Geological understandings and exploration prospects of carbonate reservoirs in Gucheng area, Tadong, Tarim Basin[J]. China Petroleum Exploration, 2020, 25(3): 96-106.
[14] 张友, 李强, 郑兴平, 等. 塔里木盆地东部古城—肖塘地区寒武纪—奥陶纪台地类型、演化过程及有利储集相带[J]. 石油学报, 2021, 42(4): 447-465.
ZHANG You, LI Qiang, ZHENG Xingping, et al.Types, evolution and favorable reservoir facies belts in the Cambrian-Ordovician platform in Gucheng-Xiaotang area, eastern Tarim Basin[J]. Acta Petrolei Sinica, 2021, 42(4): 447-465.
[15] 贺锋, 林畅松, 刘景彦, 等. 塔东南寒武系-中下奥陶统碳酸盐岩台缘带的迁移与相对海平面变化的关系[J]. 石油与天然气地质, 2017, 38(4): 711-721.
HE Feng, LIN Changsong, LIU Jingyan, et al.Migration of the Cambrian and Middle-Lower Ordovician carbonate platform margin and its relation to relative sea level changes in southeastern Tarim Basin[J]. Oil & Gas Geology, 2017, 38(4): 711-721.
[16] 张君龙. 碳酸盐岩层序沉积演化及海平面的控制作用: 以塔里木盆地古城地区奥陶系为例[J]. 天然气工业, 2017, 37(1): 46-53.
ZHANG Junlong.Carbonate sequence sedimentary evolution and control of sea level: A case study of Ordovician in the Gucheng area, Tarim Basin[J]. Natural Gas Industry, 2017, 37(1): 46-53.
[17] 张元高, 潘文庆, 唐雨, 等. 塔里木盆地古城地区下奥陶统孔隙型白云岩储层成因及演化[J]. 海相油气地质, 2024, 29(3): 236-246.
ZHANG Yuangao, PAN Wenqing, TANG Yu, et al.The genesis and evolution of porous-type dolomite reservoir of the Lower Ordovician in Gucheng area, Tarim Basin[J]. Marine Origin Petroleum Geology, 2024, 29(3): 236-246.
[18] 杜金虎, 杨华, 徐春春, 等. 东西伯利亚地台碳酸盐岩成藏条件对我国油气勘探的启示[J]. 岩性油气藏, 2013, 25(3): 1-8.
DU Jinhu, YANG Hua, XU Chunchun, et al.Carbonate reservoir forming conditions of East Siberia platform and its inspiration to oil and gas exploration in China[J]. Lithologic Reservoirs, 2013, 25(3): 1-8.
[19] 何光玉, 曹自成, 姚泽伟, 等. 塔里木盆地古城地区古生界垒-扭叠合复合断层-裂缝体模型[J]. 石油与天然气地质, 2021, 42(3): 587-594.
HE Guangyu, CAO Zicheng, YAO Zewei, et al.Paleozoic horst-twist superimposed fault-fracture body model in Gucheng area of Tarim Basin[J]. Oil & Gas Geology, 2021, 42(3): 587-594.
[20] 王招明, 杨海军, 齐英敏, 等. 塔里木盆地古城地区奥陶系天然气勘探重大突破及其启示[J]. 天然气工业, 2014, 34(1): 1-9.
WANG Zhaoming, YANG Haijun, QI Yingmin, et al.Ordovician gas exploration breakthrough in the Gucheng lower uplift of the Tarim Basin and its enlightenment[J]. Natural Gas Industry, 2014, 34(1): 1-9.
[21] 曾联波, 宋逸辰, 韩俊, 等. 塔里木盆地构造流体作用对超深层断控碳酸盐岩缝洞型储层的控制[J]. 石油勘探与开发, 2025, 52(01): 128-139.
ZENG Lianbo, SONG Yichen, HAN Jun, et al.Control of structure and fluid on ultra-deep fault-controlled carbonatefracture-vug reservoirs in Tarim Basin, NW China[J]. Petroleum Exploration and Development, 2025, 52(1): 128-139.
[22] 刘洋, 冯军, 徐伟, 等. 塔里木盆地古城地区走滑断裂特征及其对白云岩气藏的控制作用[J]. 中国石油勘探, 2022, 27(4): 135-148.
LIU Yang, FENG Jun, XU Wei, et al.Characteristics of strike slip faults and their control on dolomite gas reservoirs in Gucheng area, Tarim Basin[J]. China Petroleum Exploration, 2022, 27(4): 135-148.
[23] 刘策, 张义杰, 李洪辉, 等. 塔里木盆地古城地区奥陶系鹰山组层序地层划分及其地质意义[J]. 东北石油大学学报, 2017, 41(1): 82-96.
LIU Ce, ZHANG Yijie, LI Honghui, et al.Sequence stratigraphy classification and its geologic implications of Ordovician Yingshan Formation in Gucheng area, Tarim Basin[J]. Journal of Northeast Petroleum University, 2017, 41(1): 82-96.
[24] 曹彦清, 张友, 沈安江, 等. 塔里木盆地古城地区奥陶系碳酸盐岩成储与油气成藏[J]. 海相油气地质, 2020, 25(4): 303-311.
CAO Yanqing, ZHANG You, SHEN Anjiang, et al.Carbonate reservoir formation and hydrocarbon accumulation of Ordovician in Gucheng area, Tarim Basin[J]. Marine Origin Petroleum Geology, 2020, 25(4): 303-311.
[25] 刘红, 冯子辉, 邵红梅, 等. U-Pb同位素定年分析在热液对白云岩储层改造研究中的应用: 以塔里木盆地古城地区下奥陶统鹰三段为例[J]. 岩石学报, 2022, 38(3): 765-776.
LIU Hong, FENG Zihui, SHAO Hongmei, et al.Application of U-Pb dating technique in the study of hydrothermal activities of dolomite reservoir: A case study on 3rd member of Yingshan Formation in Gucheng area, Tarim Basin, NW China[J]. Acta Petrologica Sinica, 2022, 38(3): 765-776.
[26] 沈安江, 罗宪婴, 胡安平, 等. 从准同生到埋藏环境的白云石化路径及其成储效应[J]. 石油勘探与开发, 2022, 49(4): 637-647.
SHEN Anjiang, LUO Xianying, HU Anping, et al.Dolomitization evolution and its effects on hydrocarbon reservoir formation from penecontemporaneous to deep burial environment[J]. Petroleum Exploration and Development, 2022, 49(4): 637-647.
[27] ZHAO D F, NI C, LI S R, et al.Dolomitization history and fluid evolution of end-Ediacaran multi-phase dolomites from the near- surface to deep burial depths in the Tarim craton, northwestern China[J]. Marine and Petroleum Geology, 2024, 168: 106929.
[28] 程婷, ZHAO Jianxin, FENG Yuexing, 等. 低铀碳酸盐矿物的LA-MC-ICPMS微区原位U-Pb定年方法[J]. 科学通报, 2020, 65(2/3): 150-154.
CHENG Ting, ZHAO Jianxin, FENG Yuexing, et al.In-situ LA-MC-ICPMS U-Pb dating method for low-uranium carbonate minerals[J]. Chinese Science Bulletin, 2020, 65(2/3): 150-154.
[29] PATON C, HELLSTROM J, PAUL B, et al.Iolite: Freeware for the visualisation and processing of mass spectrometric data[J]. Journal of Analytical Atomic Spectrometry, 2011, 26(12): 2508-2518.
[30] WIEDENBECK M, ALLÉ P, CORFU F, et al.Three natural zircon standards for U-Th-Pb, Lu-Hf, trace element and REE analyses[J]. Geostandards Newsletter, 1995, 19(1): 1-23.
[31] HU Z C, LI X H, LUO T, et al.Tanz zircon megacrysts: A new zircon reference material for the microbeam determination of U-Pb ages and Zr-O isotopes[J]. Journal of Analytical Atomic Spectrometry, 2021, 36(12): 2715-2734.
[32] WU S T, YANG Y H, Nick M.W, et al. In situ calcite U-Pb geochronology by high-sensitivity single-collector LA-SF-ICP-MS[J]. SCIENCE CHINA Earth Sciences, 2022, 65(6): 1146-1160.
[33] MELIM L A, SWART P K, MALIVA R G.Meteoric-like fabrics forming in marine waters: Implications for the use of petrography to identify diagenetic environments[J]. Geology, 1995, 23(8): 755-758.
[34] 余宽宏, 金振奎. 地震相在塔里木盆地古城地区碳酸盐岩台地演化及特征分析中的应用[J]. 天然气地球科学, 2011, 22(1): 115-121.
YU Kuanhong, JIN Zhenkui.Application of seismic facies analysis method in studies of evolution and characteristics of Gucheng platform in Tarim Basin[J]. Natural Gas Geoscience, 2011, 22(1): 115-121.
[35] MUÑOZ-LÓPEZ D, KOESHIDAYATULLAH A, BOVER-ARNAL T, et al. Isotope record of Aptian third-order sea-level trends in platform margin carbonates: Implications for sequence stratigraphic analysis[J]. Journal of Sedimentary Research, 2025, 95(2): 417-433.
[36] 朱金富, 于炳松, 黄文辉, 等. 塔里木盆地塔中地区晚寒武世-奥陶世碳酸盐岩碳、氧同位素特征[J]. 大庆石油地质与开发, 2008, 27(1): 39-42.
ZHU Jinfu, YU Bingsong, HUANG Wenhui, et al.Carbon and oxygen isotope features of Late Cambrian-Ordovician in central Tarim Basin[J]. Petroleum Geology & Oilfield Development in Daqing, 2008, 27(1): 39-42.
[37] 鲍志东, 金之钧, 孙龙德, 等. 塔里木地区早古生代海平面波动特征: 来自地球化学及岩溶的证据[J]. 地质学报, 2006, 80(3): 366-373.
BAO Zhidong, JIN Zhijun, SUN Longde, et al.Sea-level fluctuation of the Tarim area in the Early Paleozoic: Respondence from geochemistry and karst[J]. Acta Geologica Sinica, 2006, 80(3): 366-373.
[38] 赵宗举. 全球海平面变化指标及海相构造层序研究方法: 以塔里木盆地奥陶系为例[J]. 石油学报, 2015, 36(3): 262-273.
ZHAO Zongju.Indicators of global sea-level change and research methods of marine tectonic sequences: Take Ordovician of Tarim Basin as an example[J]. Acta Petrolei Sinica, 2015, 36(3): 262-273.
[39] 万洋, 李峰峰, 任立新, 等. 弱局限沉积环境下碳酸盐岩特征及有利储层成因: 以中阿拉伯盆地 A 油田下白垩统 Yamama 组为例[J]. 石油勘探与开发, 2024, 51(5): 1-15.
WAN Yang, LI Feng, REN Lixin, et al.Carbonate rock characteristics and favorable reservoir origin in a slightly restricteddepositional setting: A case study of Lower Cretaceous Yamama Formation in Oilfield A, Central Arabian Basin[J]. PetroleumExploration and Development, 2024, 51(5): 1-15.
[40] WILSON J L.Carbonate facies in geologic history[M]. New York: Springer, 1975.
[41] KENTER J A M. Carbonate platform flanks: Slope angle and sediment fabric[J]. Sedimentology, 1990, 37(5): 777-794.
[42] JO A, EBERLI G P, GRASMUECK M.Margin collapse and slope failure along southwestern Great Bahama Bank[J]. Sedimentary Geology, 2015, 317: 43-52.
[43] LIU G, WU S G, GAO J W, et al.Seismic architecture of Yongle isolated carbonate platform in Xisha Archipelago, South China Sea[J]. Frontiers in Earth Science, 2023, 11: 1100675.
[44] 谭秀成, 何如意, 杨文杰, 等. 四川盆地武胜—潼南地区中二叠统茅口组二段下亚段白云岩薄储层成因及分布模式[J]. 石油勘探与开发, 2025, 52(1): 112-127.
TAN Xiucheng, HE Ruyi, YANG Wenjie, et al.Origin and distribution model of thin dolomite reservoirs in the lowersub-member of Mao 2 Member of Middle Permian Maokou Formation in Wusheng-Tongnan area, Sichuan Basin, SWChina[J]. Petroleum Exploration and Development, 2025, 52(1): 112-127.