湖相碳酸盐岩礁滩体系沉积特征、主控因素及成因模式: 以东营凹陷西部沙四上亚段为例<sup>*</sup>

doi:10.7605/gdlxb.2023.04.064

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Abstract

Lacustrine carbonates are widely distributed in continental lacustrine basins. The development model of a large reef-shoal depositional system is of great significance for understanding the genetic mechanism of lacustrine carbonates. Based on drilling cores,thin sections,well-log,seismic data and geochemistry measurements,the sedimentary characteristics of lacustrine carbonates in the upper Member 4 of Shahejie Formation(Es^s₄)of the Dongying sag were analyzed in detail. The results show that seven rock types and four lithologic assemblages were developed in the study area,and four types of sedimentary microfacies, including algal reef,shallow shoal,mudflat and storm deposits can be identified. The algal reef and shallow shoal constitute the reef-shoal complex depositional system,which was mainly distributed in the NE-SW direction of the top of the carbonate platform. The mudflat was mainly developed in the platform and near the denudation area,while the storm deposits were distributed in the upper part of the southeast slope of the platform. From the early to late stage of the highstand period,the reef-shoal complex system gradually migrated laterally from the former vertical accretion,and the plane distribution gradually expanded to the upper part of the slope area. It was speculated that the warm climate,the prevailing southeast wind of the palaeo-East Asian monsoon climate,basin structure and palaeogeomorphology,lake level fluctuation,carbonate weathering and seawater transgression integrated controlled the formation and evolution of the lacustrine reef-shoal system. The “climate-provenance-basin”genetic model for lacustrine carbonates was proposed in this paper,which can enrich the understanding of the formation mechanism of large-scale reef-shoal depositional system in lacustrine basins.

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	Articles by authors
	LIU Shengqian
	HE Youbin
	JIANG Zaixing
	LUO Jinxiong
	ZHU Xueqing
	ZHU Qing
	TANG Wei

Key words： Dongying sag Shahejie Formation lacustrine carbonates reef-shoal depositional system palaeo-East Asian monsoon depositional model

Received: 27 March 2023

ZTFLH:

P512.2

Fund:

Financially supported by the National Natural Science Foundation of China(No.41902117)

About author: LIU Shengqian,born in 1990,associate professor,is engaged in research and teaching on sedimentology. E-mail: liusq@yangtzeu.edu.cn.

Cite this article:

LIU Shengqian,HE Youbin,JIANG Zaixing et al. Sedimentary characteristics, dominant factors and genetic model of lacustrine carbonate reef-shoal depositional system: a case study from the upper 4^th Member of Shahejie Formation in western Dongying sag[J]. JOPC, 2023, 25(4): 872-888.

URL:

http://journal09.magtechjournal.com/gdlxb/EN/10.7605/gdlxb.2023.04.064 OR http://journal09.magtechjournal.com/gdlxb/EN/Y2023/V25/I4/872

[1] 陈笑夜,曹剑,施春华,边立曾. 2012. 陆相湖盆海侵地质事件识别及其对烃源岩形成影响. 地质论评, 58(5): 901-910.
[Chen X Y,Cao J,Shi C H,Bian L Z.2012. A review on the distinguishing of marine transgression in continental basins and its impacts on the formation of hydrocarbon source rocks. Geological Review, 58(5): 901-910]
[2] 杜韫华. 1990. 渤海湾地区下第三系湖相碳酸盐岩及沉积模式. 石油与天然气地质, 11(4): 376-392,465-466.
[Du Y H.1990. Eogene lacustrine carbonate rocks and sedimentary model in Boha1 Bay Region. Oil & Gas Geology, 11(4): 376-392,465-466]
[3] 冯磊,姜在兴,田继军. 2009. 东营凹陷沙四上亚段层序地层格架研究. 特种油气藏, 16(1): 16-19,106.
[Feng L,Jiang Z X,Tian J J.2009. Sequence stratigraphy framework of sub-Es4u in Dongying Depression. Special Oil and Gas Reservoir, 16(1): 16-19,106]
[4] 高晓鹏. 2012. 沾车地区沙四上亚段湖相碳酸盐岩沉积特征研究. 北京: 中国地质大学(北京)博士论文.
[Gao X P.2012. The sedimentologic characteristics of lacustrine carbonate rocks in the upper 4th member of Shahejie Formation,Zhanhua and Chezhen area. Beijing:Doctoral dissertation of China University of Geosciences(Beijing)]
[5] 何赛,李国蓉,吴昌荣,刘树根,张忠民,苏玉山,朱奕璇,何钊,任杰,王雨辰,周伟,王亚. 2022. 巴西桑托斯盆地湖相微生物碳酸盐岩层序沉积特征及控制因素. 石油勘探与开发, 49(4): 683-692.
[He S,Li G R,Wu C R,Liu S G,Zhang Z M,Su Y S,Zhu Y X,He Z,Ren J,Wang Y C,Zhou W,Wang Y J.2022. Sedimentary filling characteristics and controlling factors of lacustrine microbial carbonates sequence in the Santos Basin,Brazil. Petroleum Exploration and Development, 49(4): 683-692]
[6] 侯启军,何海清,李建忠,杨涛. 2018. 中国石油天然气股份有限公司近期油气勘探进展及前景展望. 中国石油勘探, 23(1): 1-13.
[Hou Q J,He H Q,Li J Z,Yang T.2018. Recent progress and prospect of oil and gas exploration by PetroChina Company Limited. China Petroleum Exploration, 23(1): 1-13]
[7] 纪友亮,马达德,薛建勤,王鹏,吴颜雄,曾力,金力. 2017. 柴达木盆地西部新生界陆相湖盆碳酸盐岩沉积环境与沉积模式. 古地理学报, 19(5): 757-772.
[Ji Y L,Ma D D,Xue J Q,Wang P,Wu Y X,Zeng L,Jin L.2017. Sedimentary environments and sedimentary model of carbonate rocks in the Cenozoic lacustrine basin,western Qaidam Basin. Journal of Palaeogeography(Chinese Edtion), 19(5): 757-772]
[8] 贾怀存,康洪全,梁建设,程涛,张世鑫. 2021. 桑托斯盆地湖相碳酸盐岩储层特征及控制因素. 西南石油大学学报(自然科学版), 43(2): 1-9.
[Jia H C,Kang H Q,Liang J S,Cheng T,Zhang S X.2021. Characteristic and developmental controlled factors of pre-salt lacustrine carbonate,Santos Basin. Journal of Southwest Petroleum University(Science &Technology Edition), 43(2): 1-9]
[9] 姜秀芳. 2010. 济阳坳陷沙四段湖相碳酸盐岩分布规律及沉积模式. 油气地质与采收率, 17(6): 12-15,111.
[Jiang X F.2010. The distribution pattern and sedimentary mode of the carbonate rock in Sha4 member in Jiyang depression. Petroleum Geology and Recovery Efficiency, 17(6): 12-15,111]
[10] 姜秀芳. 2011. 济阳坳陷湖相碳酸盐岩沉积主控因素. 油气地质与采收率, 18(6): 23-27,112.
[Jiang X F.2011. Main controlling factors of lacustrine carbonate rock in Jiyang depression. Petroleum Geology and Recovery Efficiency, 18(6): 23-27,112]
[11] 姜在兴,王雯雯,王俊辉,李庆,张元福. 2017. 风动力场对沉积体系的作用. 沉积学报, 35(5): 863-876.
[Jiang Z X,Wang W W,Wang J H,Li Q,Zhang Y F.2017. The Influence of wind field on depositional system. Acta Sedimentologica Sinica, 35(5): 863-876]
[12] 姜在兴. 2016. 风场—物源—盆地系统沉积动力学: 沉积体系成因解释与分部预测新概念. 北京: 科学出版社,1-256.
[Jiang Z X.2016. Sedimentary Dynamics of Windfield-Source-Basin System: New Concept for Interpretation and Prediction. Beijing: Science Press,1-256]
[13] 李国欣,张永庶,陈琰,张国卿,雷涛. 2022. 柴达木盆地油气勘探进展、方向与对策. 中国石油勘探, 27(3): 1-19.
[Li G X,Zhang Y S,Chen Y,Zhang G Q,Lei T.2022. Progress,orientation and countermeasures of petroleum exploration in Qaidam Basin. China Petroleum Exploration, 27(3): 1-19]
[14] 李勇,钟建华,温志峰,王海侨. 2006. 济阳坳陷古近系湖相生物礁油气藏研究. 沉积学报, 24(1): 56-67.
[Li Y,Zhong J H,Wen Z F,Wang H Q.2006. The study on the Palaeogene lacustrine reefs in Jiyang sag eastern Shandong Province. Acta Sedimentologica Sinica, 24(1): 56-67]
[15] 林畅松,刘景彦,张英志,胡博. 2005. 构造活动盆地的层序地层与构造地层分析: 以中国中、新生代构造活动湖盆分析为例. 地学前缘, 12(4): 365-374.
[Lin C S,Liu J Y,Zhang Y Z,Hu B.2005. Sequence stratigraphy and tectono-stratigraphic analysis of tectonically active basins: a case study on the Cenozoic-Mesozoic lacustrine basins in China. Earth Science Frontiers, 12(4): 365-374]
[16] 刘传联,成鑫荣. 1996. 渤海湾盆地早第三纪非海相钙质超微化石的锶同位素证据. 科学通报, 41(10): 908-910.
[Liu C L,Cheng X R.1996. Strontium isotope evidence of early Tertiary non-marine calcareous nannofossils in Bohai Bay Basin. Chinese Science Bulletin, 41(10): 908-910]
[17] 刘传联,赵泉鸿,汪品先. 2002. 从化石群及壳体同位素看古近纪东营湖湖水化学. 地球学报, 23(3): 237-242.
[Liu C L,Zhao Q H,Wang P X.2002. Water chemistry of the Paleogene Dongying lake: evidence from fossil assemblages and shell isotopes. Acta Geoscientia Sinica, 23(3): 237-242]
[18] 刘圣乾. 2018. 东营凹陷西部沙四上亚段湖相碳酸盐岩沉积特征研究. 北京: 中国地质大学(北京)博士论文.
[Liu S Q.2018. Sedimentary characteristics of lacustrine carbonates in the upper fourth member of Shahejie Formation(Es4s),western Dongying Depression. Beijing:Doctoral dissertation of China University of Geosciences(Beijing)]
[19] 马义权. 2017. 济阳坳陷古近系沙河街组湖相页岩岩相学及古气候记录.中国地质大学(武汉)博士论文.
[Ma Y Q.2017. Lacustrine shale stratigraphy and Eocene climate recorded in the Jiyang Depression in East China. Doctoral dissertation of China University of Geosciences(Wuhan)]
[20] 彭世福. 1992. 中国近海早第三纪海侵层序及地层对比. 海洋地质与第四纪地质, 12(1): 41-56.
[Peng S F.1992. Tertiary transgressive sequences and stratigraphic correlation in China offshore area. Marine Geology & Quaternary Geology, 12(1): 41-56]
[21] 钱凯,王素民,刘淑范,时华星. 1980. 华东北部下第三系礁灰岩的发现及其石油地质意义. 科学通报,(24): 1140-1142.
[Qian K,Wang S M,Liu S F,Shi H X.1980. Discovery of lower Tertiary reef limestone in east China and its petroleum geological significance. Chinese Science Bulletin,(24): 1140-1142]
[22] 邵龙义. 1994. 碳酸盐岩氧、碳同位素与古温度等的关系. 中国矿业大学学报, 23(1): 39-45.
[Shao L Y.1994. The relation of the oxygen and carbon isotope in the carbonate rocks to the paleotemperature etc. Journal of China University of Mining & Technology, 23(1): 39-45]
[23] 申培旸,刘震,刘诗敏,马立驰,孙超,李自远,杨晓光,卢朝进. 2018. 沾化凹陷长堤地区沙一段生物灰岩发育模式及分布特征. 沉积学报, 36(5): 995-1007.
[Shen P Y,Liu Z,Liu S M,Ma L C,Sun C,Li Z Y,Yang X G,Lu C J.2018. Developing pattern and distribution features of biological limestone in first member of Shahejie Formation in Changdi area,Zhanhua Depression,Bohai Bay Basin,China. Acta Sedimentologica Sinica, 36(5): 995-1007]
[24] 宋国奇,王延章,石小虎,路达,闫瑞萍. 2013. 东营沙四段古盐度对碳酸盐岩沉积的控制作用. 西南石油大学学报(自然科学版), 35(2): 8-14.
[Song G Q,Wang Y Z,Shi X H,Lu D,Yan R P.2013. Palaeosalinity and its controlling on the development of beach and bar in lake facies. Journal of Southwest Petroleum University(Science &Technology Edition), 35(2): 8-14]
[25] 苏玲,朱如凯,崔景伟,吴松涛,罗忠,毛治国,李森. 2017. 中国湖相碳酸盐岩时空分布与碳氧同位素特征. 古地理学报, 19(6): 1063-1074.
[Su L,Zhu R K,Cui J W,Wu S T,Luo Z,Mao Z G,Li S.2017. Spatial-temporal distribution of lacustrine carbonate rocks in China and their carbon and oxygen isotopic characteristics. Journal of Palaeogeography(Chinese Edition), 19(6): 1063-1074]
[26] 唐鑫萍,雷栋,宋效文. 2021. 三水盆地布心组湖相碳酸盐岩沉积特征及相模式. 天然气地球科学, 32(5): 675-684.
[Tang X P,Lei D,Song X W.2021. Sedimentary characteristics and facies model of lacustrine carbonate rocks of Buxin Formation,Sanshui Basin. Natural Gas Geoscience, 32(5): 675-684]
[27] 田继军,姜在兴. 2009. 东营凹陷沙河街组四段上亚段层序地层特征与沉积体系演化. 地质学报, 83(6): 836-846.
[Tian J J,Jiang Z X.2009. Sequence stratigraphy characteristics and sedimentary system evolution of upper Es₄ in the Dongying Depression. Acta Geologica Sinica, 83(6): 836-846]
[28] 汪品先,闵秋宝,卞云华. 1982. 关于我国东部含油盆地早第三纪地层的沉积环境. 地质论评, 28(5): 12-22.
[Wang P X,Min Q B,Bian Y H.1982. On the sedimentary environments of the Paleogene strata in oil-bearing basins in the eastern part of China. Geological Review, 28(5): 12-22]
[29] 王东,王国芝,郝雪峰,石砥石,姜秀芳. 2009. 东营凹陷沙四段碳酸盐岩稀土元素地球化学特征. 沉积与特提斯地质, 29(4): 62-67.
[Wang D,Wang G Z,Hao X F,Shi D S,Jiang X F.2009. REE geochemistry of the carbonate rocks from the 4th member of the Shahejie Formation in the Dongying depression,Shangdong. Sedimentary Geology and Tethyan Geology, 29(4): 62-67]
[30] 王冠民,林国松. 2012. 济阳坳陷古近纪的古气候区分析. 矿物岩石地球化学通报, 31(5): 505-509.
[Wang G M,Lin G S.2012. Eogene paleoclimate zone study in the Jiyang Depression. Bulletin of Mineralogy,Petrology and Geochemistry, 31(5): 505-509]
[31] 王夕宾,郝延征,姚军,张建光,吕爱民. 2016. 东营凹陷沙一段薄层湖相碳酸盐岩成因研究. 中国石油大学学报(自然科学版), 40(1): 27-34.
[Wang X B,Hao Y Z,Yao J,Zhang J G,Lü A M.2016. Genetic research of flaggy lacustrine carbonate in the first member of Shahejie Formation,Dongying Depression. Journal of China University of Petroleum(Edition of Natural Science), 40(1): 27-34]
[32] 王英华,周书欣,张秀莲. 1993. 中国湖相碳酸盐岩. 徐州: 中国矿业大学出版社,1-131.
[Wang Y H,Zhou S X,Zhang X L.1993. Lacustrine Carbonate Rocks in China. Xuzhou: China University of Mining and Technology Press,1-131]
[33] 王颖,王晓州,廖计华,朱石磊,蔡露露. 2016. 巴西桑托斯盆地白垩系湖相藻叠层石礁特征及主控因素分析. 沉积学报, 34(5): 819-829.
[Wang Y,Wang X Z,Liao J H,Zhu S L,Cai L L.2016. Cretaceous lacustrine algal stromatolite reef characteristics and controlling factors,Santos Basin,Brazil. Acta Sedimentologica Sinica, 34(5): 819-829.
[34] 吴靖,姜在兴,钱侃,徐丹. 2014. 山东省东营凹陷沙四上亚段咸化机制特征. 地球学报, 35(6): 733-740.
[Wu J,Jiang Z X,Qian K,Xu D.2014. Characteristics of salinization mechanism on the upper part of Fourth Member of Shahejie Formation in the Dongying sag,Shandong Province. Acta Geoscientica Sinica, 35(6): 733-740]
[35] 杨勇强,邱隆伟,姜在兴,白凤坤. 2011. 东营凹陷沙四上亚段滩坝物源体系. 吉林大学学报(地球科学版), 41(1): 46-53.
[Yang Y Q,Qiu L W,Jiang Z X,Bai F K.2011. Beach bar provenance system on the upper part of fourth member of Shahejie Formation,in Dongying Sag. Journal of Jilin University(Earth Science Edition), 41(1): 46-53]
[36] 伊海生,林金辉,周恳恳,李军鹏,黄华谷. 2008. 可可西里地区中新世湖相叠层石成因及其古气候意义. 矿物岩石, 28(1): 106-113.
[Yi H S,Lin J H,Zhou K K,Li J P,Huang H G.2008. The origin of Miocene lacustrine stromatolites in the Hoh-xil area and its paleoclimatic implications. Journal of Mineral Petrology, 28(1): 106-113]
[37] 袁文芳,陈世悦,曾昌民. 2006. 济阳坳陷古近系沙河街组海侵问题研究. 石油学报, 27(4): 40-44,49.
[Yuan W F,Chen S Y,Zeng C M.2006. Study on marine transgression of Paleogene Shahejie Formation in Jiyang Depression. Acta Petrolei Sinica, 27(4): 40-44,49]
[38] 张忠民,朱奕璇,张德民,苏玉山,姚威,鲍志东,宋健,沈卫宏. 2020. 巴西大坎波斯盆地盐下碳酸盐岩油气成藏规律与勘探启示. 中国石油勘探, 25(4): 75-85.
[Zhang Z M,Zhu Y X,Zhang D M,Su Y S,Yao W,Bao Z D,Song J,Shen W H.2020. Hydrocarbon accumulation rules and exploration inspiration of pre-salt carbonate reservoirs in the Great Campos Basin,Brazil. China Petroleum Exploration, 25(4): 75-85]
[39] 赵澄林. 2001. 油区岩相古地理. 山东东营: 石油大学出版社,1-314.
[Zhao C L.2001. Lithofacies Palaeogeography of Oil Field. Shandong Dongying: Petroleum University Press,1-314]
[40] 赵兰全. 2022. 咸化湖盆缓坡带碳酸盐岩岩石学特征及沉积模式: 以东营凹陷古近系沙四上亚段为例. 西安石油大学学报(自然科学版), 37(4): 10-16,35.
[Zhao L Q.2022. Petrological characteristics and sedimentary mode of salinized lacustrine carbonate: a case study on upper part of the fourth member of Shahejie Formation in Dongying sag. Journal of Xi'an Shiyou University(Natural Science Edition), 37(4): 10-16,35]
[41] 朱超,刘占国,宋光永,龙国徽,宫清顺,赵健,李森明,夏志远,吴颜雄,田明智. 2022. 柴达木盆地英雄岭构造带古近系湖相碳酸盐岩沉积模式、演化与分布. 石油学报, 43(11): 1558-1567,1622.
[Zhu C,Liu Z G,Song G Y,Long G H,Gong Q S,Zhao J,Li S M,Xia Z Y,Wu Y X,Tian M Z.2022. Sedimentary model,evolution and distribution of Paleogene lacustrine carbonate rocks in Yingxiongling structural belt,Qaidam Basin. Acta Petrolei Sinica, 43(11): 1558-1567,1622]
[42] Craig H.1965. The measurement of oxygen isotope paleotemperatures. In: Tongiorgi E(ed). Stable Isotopes in Oceanographic Studies and Paleotemperature. Pisa: Consiglio Nazionale delle Ricerche Laboratorio di Geologia Nucleare,161-182.
[43] Flügel E.2010. Microfacies of Carbonate Rocks: Analysis,Interpretation and Application. Berlin Heidelberg: Springer-Verlag,369-398.
[44] Gierlowski-Kordesch E H.2010. Chapter 1: Lacustrine Carbonates. Developments in Sedimentology, 61: 1-101.
[45] Huber M,Golder A.2012. Eocene monsoons. Journal of Asian Earth Sciences, 44: 3-23.
[46] Licht A,van-Cappelle M,Abels H A,Ladant J B,Alexandre J T,Lanord C F,Donnadieu Y,Wagonerdenberghe J,Rigaudier T,Lécuyer C,Terry Jr D,Adroaens R,Boura A,Soe A N,Quade J,Nivet G D,Jaeger J J.2014. Asian monsoons in a late Eocene greenhouse world. Nature, 513: 501-506.
[47] Liu S,Jiang Z,He Y,Dou L,Yang Y,Li Y,Han C.2020. Geomorphology,lithofacies and sedimentary environment of lacustrine carbonates in the Eocene Dongying Depression,Bohai Bay Basin,China. Marine and Petroleum Geology, 113: 104125.
[48] Meng Q,Bruch A A,Sun G,Liu Z,Hu F,Sun P.2018. Quantitative reconstruction of Middle and Late Eocene paleoclimate based on palynological records from the Huadian Basin,northeastern China: evidence for monsoonal influence on oil shale formation. Palaeogeography,Palaeoclimatology,Palaeoecology, 510: 63-77.
[49] Miller K G,Kominz M A,Browning J V,Wright J D,Mountain G S,Katz M E,Sugarman P J,Cramer B S,Christie-Blick N,Pekar S F.2005. The Phanerozoic record of global sea-level change. Science, 310(25): 1293-1298.
[50] Muniz M C,Bosence D W J.2018. Lacustrine carbonate platforms: facies,cycles,and tectonosedimentary models for the presalt Lagoa Feia Group(lower Cretaceous),Campos Basin,Brazil. AAPG Bulletin, 102(12): 2569-2597.
[51] Olivito J P R,Souza F J.2020. Depositional model of Early Cretaceous lacustrine carbonate reservoirs of the Coqueiros Formation-northern Campos Basin,southeastern Brazil. Marine and Petroleum Geology, 111: 414-439.
[52] Platt N H,Wright V P.1991. Lacustrine carbonates: facies models,facies distributions and hydrocarbon aspects. Special publications of International Association of Sedimentologist, 13: 57-74.
[53] Quan C,Liu C,Utescher T.2011. Paleogene evolution of precipitation in northeastern China supporting the Middle Eocene intensification of the East Asian monsoon. Palaios, 26: 743-753.
[54] Wang J,Jiang Z,Xian B,Chen J,Wang X,Xu W.2018. A method to define the palaeowind strength from lacustrine parameters. Sedimentology, 65: 461-491.
[55] Wang J,Jiang Z,Zhang Y.2015. Subsurface lacustrine storm-seiche depositional model in the Eocene Lijin sag of the Bohai Bay Basin,East China. Sedimentary Geology, 328: 55-72.
[56] Wang Q,Spicer R A,Yang J,Wang Y,Li C.2013. The Eocene climate of China,the early elevation of the Tibetan Plateau and the onset of the Asian Monsoon. Global Change Biology, 19: 3709-3728.
[57] Wright V P.1992. A revised classification of limestones. Sedimentary Geology, 76(3-4): 177-185.
[58] Wu J,Liang C,Yang R,Xie J.2022. Variation of lacustrine carbonate deposition in the Eocene Dongying Depression and its comparison with Holocene environments. Geological Magazine, 159(6): 963-980.
[59] Xue X,Zhang Y,Jiang Z,Wang L,Jiang H.2021. Wave and storm signals in a lacustrine succession and their relationship to paleowind direction(Tanan Depression,Mongolia,early Cretaceous). Sedimentary Geology, 419: 105911.
[60] Zachos J C,Dickens G R,Zeebe R E.2008. An Early Cenozoic perspective on greenhouse warming and carbon-cycle dynamics. Nature, 451(17): 279-283.