山东东部白垩系莱阳群沉积地层与有机质特征
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摘要
为了解山东东部白垩系莱阳群沉积地层,研究有机质特征,在对灵山岛、崂山垭口—八仙墩及胶莱盆地的典型剖面地层野外踏勘的基础上,结合灵山岛元素地球化学、胶莱盆地有机地球化学的相关研究成果,采用了沉积学、沉积地球化学、有机地球化学的研究方法手段,系统研究了灵山岛莱阳群地层的有机质特征。胶莱盆地早白垩世莱阳期主要发育一套河湖相及冲积扇相的陆相沉积地层,有机地球化学研究表明,其水南段烃源岩样品主要为腐泥型(Ⅰ型)和腐殖腐泥型(Ⅱ_1型),已进入生烃门限,处于热演化成熟阶段;而灵山岛、崂山垭口-八仙墩早白垩世莱阳期则主要发育深水重力流、深水牵引流为主的海相沉积地层,对灵山岛粉砂岩和页岩进行元素地球化学研究指示了其沉积环境为海相还原环境,且有机地球化学研究表明,灵山岛样品为腐殖型(Ⅲ型)和腐殖腐泥型(Ⅱ1型),处于高成熟到过成熟阶段,灵山岛浊积岩可能已经完成了生排烃过程。
The organic matter features of the Laiyang Group in Lingshan Island were systematically studied by means of sedimentology,sedimentary geochemistry and organic geochemistry and integrating with typical outcrop observation in Lingshan Island,Laoshan Yakou-Baxiandun area and Jiaolai Basin and the previous research on the elemental geochemistry of Lingshan Island and the organic geochemistry of Jiaolai Basin. In Jiaolai Basin,the terrestrial strata of fluvial and lacustrine facies and alluvial fan facies were developed in the Early Cretaceous Laiyang period. The organic geochemistry studies on the deposits show that the source rock samples from the Shuinan section are mainly of saprolite( Type Ⅰ) and humus and saprolite( Type Ⅱ_1),have entered the hydrocarbon generation threshold and are in the thermal mature stage;while in the Lingshan Island,LaoshanYakou-Baxiandun areas,marine strata dominated by deep sea gravity flow and deep water traction current deposits were developed in the Early Cretaceous Laiyang period. Meanwhile the elemental geochemical studies on siltstones and shales of Lingshan Island reveal that its sedimentary setting is a marine reducing environment,and the organic geochemical research shows that samples from Lingshan Island belong to the humic( Type Ⅲ) and humic and sapropel( Type Ⅱ_1) types in high to over mature stage,and the turbidites of Lingshan Island may have completed the process of hydrocarbon generation and expulsion.
The organic matter features of the Laiyang Group in Lingshan Island were systematically studied by means of sedimentology,sedimentary geochemistry and organic geochemistry and integrating with typical outcrop observation in Lingshan Island,Laoshan Yakou-Baxiandun area and Jiaolai Basin and the previous research on the elemental geochemistry of Lingshan Island and the organic geochemistry of Jiaolai Basin. In Jiaolai Basin,the terrestrial strata of fluvial and lacustrine facies and alluvial fan facies were developed in the Early Cretaceous Laiyang period. The organic geochemistry studies on the deposits show that the source rock samples from the Shuinan section are mainly of saprolite( Type Ⅰ) and humus and saprolite( Type Ⅱ_1),have entered the hydrocarbon generation threshold and are in the thermal mature stage;while in the Lingshan Island,LaoshanYakou-Baxiandun areas,marine strata dominated by deep sea gravity flow and deep water traction current deposits were developed in the Early Cretaceous Laiyang period. Meanwhile the elemental geochemical studies on siltstones and shales of Lingshan Island reveal that its sedimentary setting is a marine reducing environment,and the organic geochemical research shows that samples from Lingshan Island belong to the humic( Type Ⅲ) and humic and sapropel( Type Ⅱ_1) types in high to over mature stage,and the turbidites of Lingshan Island may have completed the process of hydrocarbon generation and expulsion.
引文
[1]周瑶琪,张振凯,梁文栋,等.山东东部晚中生代构造-岩浆活动及原型盆地恢复[J].地学前缘,2015,22(1):137-156.Zhou Yaoqi,Zhang Zhengkai,Liang Wendong,et al. Late Mesozoic tectono-magmatic activities and prototype basin restoration in Eastern Shandong Province,China[J]. Earth Science Frontiers,2015,22(1):137-156.
[2]张振凯,周瑶琪,梁文栋,等.山东灵山岛早白垩世构造演化及地质意义[J].海洋地质前沿,2016,32(4):1-10.Zhang Zhenkai,Zhou Yaoqi,Liang Wendong,et al. Early cretaceous tectonic evolution of Lingshan Island in Shandong province and its geologic significance[J]. Marine Geology Frontiers,2016,32(4):1-10.
[3]栾光忠,李安龙,王建,等.青岛主要海岛成因分类及其地质环境分析[J].中国海洋大学学报(自然科学版),2010,40(8):111-116.Luan Guangzhong,Li Anlong,Wang Jian,et al. The geological origin division of the main sea island in Qingdao area and environment analysis[J]. Periodical of Ocean University of China,2010,40(8):111-116.
[4]吕洪波,王俊,张海春.山东灵山岛晚中生代滑塌沉积层的发现及区域构造意义初探[J].地质学报,2011,85(6):938-946.Lu Hongbo,Wang Jun,Zhang Haichun. Discovery of the late mesozoic slump beds in Lingshan Island,Shandong and a pilot research on the regional tectonics[J]. Acta Geologica Sinica,2011,85(6):938-946.
[5]吕洪波,张海春,王俊,等.山东胶南灵山岛晚中生代浊积岩中发现巨大滑积岩块[J].地质论评,2012,58(1):80-81.Lu Hongbo,Zhang Haichun,Wang Jun,et al. Giant landslides found in the Late Mesozoic turbidites in Lingshan Island,Jiaonan,Shandong[J]. Geological Review,2012,58(1):80-81.
[6]梁钊,周瑶琪.山东省灵山岛下白垩统浊积岩中与滑塌作用相关的软沉积物变形构造[J].地球科学,2017,42(10):1715-1724.Liang Zhao,Zhou Yaoqi. Soft sediment deformation structures related to slumping in Lower Cretaceous turbidite in Lingshan Island,Shandong Province[J]. Earth Science,2017,42(10):1715-1724.
[7]王安东,周瑶琪,闫华,等.山东省灵山岛早白垩世软沉积物变形构造特征[J].古地理学报,2013,15(5):717-728.Wang Andong,Zhou Yaoqi,Yan Hua,et al. Characteristics of soft sediment deformation structures of the Early Cretaceous in Lingshan Island of Shandong Province[J]. Journal of Palaeogeography,2013,15(5):717-728.
[8]邵珠福,钟建华,李勇,等.青岛灵山岛晚中生代重力流沉积特征及环境分析[J].地质论评,2014,60(3):555-566.Shao Zhufu,Zhong Jianhua,Li Yong,et al. The sedimentary characteristics and environmental analysis of Late Mesozoic gravity flows in Lingshan Island. Geological Review[J]. 2014,60(3):555-566.
[9]周瑶琪,周腾飞,张振凯,等.山东省灵山岛下白垩统青山群火山地震软沉积物变形构造特征及成因机制[J].古地理学报,2017,19(4):567-582.Zhou Yaoqi,Zhou Tengfei,Zhang Zhenkai,et al. Characteristics and formation mechanism of soft-sediment deformation structures related to volcanic earthquakes of the Lower Cretaceous Qingshan Group in Lingshan Island,Shandong Province[J]. Journal of Palaeogeography,2017,19(4):567-582.
[10] Yang R,Fan A,Han Z,et al. An upward shallowing succession of gravity flow deposits in the Early Cretaceous Lingshandao Formation,Western Yellow Sea[J]. Acta Geologica Sinica,2016,90(4):1553-1554.
[11] Liang Z,Zhou Y,Van L A J. Soft-sediment deformation structures in-duced by rapid sedimentation in Early Cretaceous turbidites,Lingshan Island,eastern China[J]. Canadian Journal of Earth Sciences,2018,55(2):118-129.
[12]于姗姗.山东东部近海晚中生代裂陷盆地沉积相研究[D].东营:中国石油大学(华东),2014.Yu Shanshan. Research on the Sedimentary Facies of Late Mesozoic Rift Basin in the Offshore Area of Eastern Shandong[D]. Dongying:China University of Petroleum(East China),2014.
[13]刘杨.山东近海地区下白垩统沉积岩有机地球化学特征[D].东营:中国石油大学(华东),2014.Liu Yang. Organic geochemical characteristics of Lower Cretaceous sedimentary in the offshore area of Shandong[D]. Dongying:China University of Petroleum(East China),2014.
[14]王安东,周瑶琪,张振凯,等.山东灵山岛莱阳群水下非构造裂缝特征及意义[J].地球学报,2014,35(3):321-328.Wang Andong,Zhou Yaoqi,Zhang Zhenkai,et al. Characteristics and significance of underwater non-tectonic cracks in Laiyang Group of Lingshan Island,Shandong Province[J]. Acta Geoscientica Sinica,2014,35(3):321-328.
[15] Wang J,Chang S C,Lu H B,et al. Detrital zircon U–Pb age constraints on Cretaceous sedimentary rocks of Lingshan Island and implications for tectonic evolution of Eastern Shandong,North China[J]. Journal of Asian Earth Sciences,2014,96:27-45.
[16]张海春,吕洪波,李建国,等.山东青岛早白垩世新地层单位——灵山岛组[J].地层学杂志,2013,37(2):216-222.Zhang Haichun,Lu Hongbo,Li Jianguo,et al. The Ling Shan Dao Formation:a new lithostratigraphic unit of the Early Cretaceous in Qingdao,Shandong,China[J]. Journal of Stratigraphy,2013,37(2):216-222.
[17]吕洪波,张海春,王俊,等.灵山岛早白垩世复理石不是陆内三角洲沉积——答钟建华教授[J].地质论评,2013,59(1):11-14.Lu Hongbo,Zhang Haichun,Wang Jun,et al. The Early Cretaceous Flysch in Lingshan Island is not an intracontinental delta deposit-Answering Professor Zhong Jianhua[J]. Geological Review,2013,59(1):11-14.
[18]钟建华.灵山岛中生代沉积岩是深水远源浊积岩、还是陆内三角洲沉积?——与吕洪波教授商榷[J].地质论评,2012,58(6):1180-1182.Zhong Jianhua. Is the Mesozoic sedimentary rock of Lingshan Island a deep-water distant turbidite or an intra-continental delta?——Discussing with Professor Lu Hongbo[J]. Geological Review,2012,58(6):1180-1182.
[19]邵珠福,钟建华,李勇,等.青岛灵山岛纹层控制的砂级颗粒支撑叠瓦构造的发现及其意义[J].中国科学:地球科学,2014,44(8):1761-1776.Shao Zhufu,Zhong Jianhua,Li Yong,et al. Characteristics and sedimentary processes of lamina-controlled sand-particle imbricate structure in deposits on Lingshan Island,Qingdao,China[J]. Science China:Earth Sciences,2014,44(8):1761-1776.
[20]杨仁超.灵山岛早白垩世重力流沉积类型与沉积环境探讨[C]∥中国地质学会.中国地质学会2015学术年会论文.北京:中国地质学会,2015.Yang Renchao. Discussion on types and sediemntary environment of the Early Cretaceous gravity flow deposits on Lingshan Island[C]∥Geological Society of China Abstract of The 2015 Annual Meeting of Geological Society of China. Beijing:The 2015 Annual Meeting of Geological Society of China,2015.
[21]刘菲菲,周瑶琪,许红,等.灵山岛成因特征、类型及其地质构造意义[J].海洋地质前沿,2016,32(3):33-40.Liu Feifei,Zhou Yaoqi,Xu Hong,et al. Origin of the Lingshan Island and Geotectonic Significance[J]. Marine Geology Frontiers,2016,32(3):33-40.
[22]李守军,张祥玉,赵秀丽,等.山东省青岛市灵山岛下白垩统中发现鱼类和叶肢介化石[J].地质论评,2017,63(1):1-6.Li Shoujun,Zhang Xiangyu,Zhao Xiuli,et al. Discovery of fish and conchostracan fossils in Lower Cretaceous in Lingshan Island,Qingdao,Shandong[J]. Geological Review,2017,63(1):1-6.
[23]张振凯,周瑶琪,彭甜明,等.山东灵山岛莱阳群粉砂岩地球化学特征及意义[J].地球科学,2017,42(3):357-377.Zhang Zhenkai,Zhou Yaoqi,Peng Tianming,et al. Geochemical characteristics and signatures of siltstones from Laiyang Group at Lingshan Island,Qingdao,Shandong[J]. Earth Science,2017,42(3):357-377.
[24]付永涛,虞子冶.青岛垭口—八仙墩变质海相碎屑岩的属性和构造指示意义[J].地质科学,2010,45(1):207-227.Fu Yongtao,Yu Ziye. Attributes and tectonic implications of the metamorphic marine clastic rocks in the Yakou-Baxiandun,Qingdao[J].Chinese Journal of Geology,2010,45(1):207-227.
[25]吴拓宇,赵淑娟,付永涛.青岛八仙墩海相碎屑岩的岩石地球化学特征及其油气研究意义[J].地质科学,2010,45(4):1156-1169.Wu Tuoyu,Zhao Shujuan,Fu Yongtao. Petrogeochemistrical characteristics and its implication for hydrocarbon of the Lower Paleozoic marine siliclastic rocks in Baxiandun,Qingdao[J]. Chinese Journal of Geology,2010,45(4):1156-1169.
[26]王俊.青岛崂山垭口白垩纪海相地层碎屑锆石U-Pb年龄[C]∥中国矿物岩石地球化学学会.中国矿物岩石地球化学学会第14届学术年会论文集,北京:中国矿物岩石地球化学学会,2013:1.Wang Jun. Cretaceous zircon U-Pb age of the Cretaceous marine strata in the Laoshan Yakou,Qingdao.[C]∥Chinese Society for Mine-ralogy,Petrology and Geochemistry. Abstract Paper of the 14th Annual meeting of the Chinese Society for Mineralogy,Petrology and Geochemistry. Beijing:Chinese Society for Mineralogy,2013:1.
[27]赵广涛,王德滋,曹钦臣.崂山花岗岩岩石地球化学与成因[J].高校地质学报,1997(1):2-4,6,9-16.Zhao Guangtao,Wang Dezi,Cao Qinchen. The geochemistry and genesis of the Laoshan granitoids,shandong province[J]. Geological Journal of China Universities,1997(1):2-4,6,9-16.
[28] Wang J,Chang S C,Lin P,et al. Evidence of Early Cretaceous transpression in the Sulu orogenic belt,eastern China[J]. Tectonophysics,2016,687(?):44-55.
[29]张岳桥,李金良,柳宗泉,等.胶莱盆地深部拆离系统及其区域构造意义[J].石油与天然气地质,2006(4):504-511.Zhang Yueqiao,Li Jinliang,Liu Zongquan,et al. Detachment systems in deep of Jiaolai basin and their regional tectonic significance[J].Oil&Gas Geology,2006(4):504-511.
[30]张岳桥,赵越,董树文,等.中国东部及邻区早白垩世裂陷盆地构造演化阶段[J].地学前缘,2004(3):123-133.Zhang Yueqiao,Zhao Yue,Dong Shuwen,et al. Tectonic evolution stages of the Early Cretaceous rift basins in Eastern China and adjacent areas and their geodynamic background[J]. Earth Science Frontiers,2004(3):123-133.
[31] Zhang Y,Dong S,Shi W. Cretaceous deformation history of the middle Tan-Lu fault zone in Shandong Province,eastern China[J]. Tectonophysics,2003,363(3-4):243-258.
[32]张岳桥,董树文,赵越,等.华北侏罗纪大地构造:综评与新认识[J].地质学报,2007(11):1462-1480.Zhang Yueqiao,Dong Shuwen,Zhao Yue,et al. Jurassic tectonics of North China:a Synthetic View[J]. Acta Geologica Sinica,2007(11):1462-1480.
[33]刘华,李凌,吴智平.胶莱盆地烃源岩分布及有机地球化学特征[J].石油实验地质,2006(6):574-580,585.Liu Hua,Li Ling,Wu Zhiping. Distribution and organic geochemical characteristics of hydrocarbon source rocks in the jiaolai basin petroleum[J]. Geology&Experiment,2006(6):574-580,585.
[34] Mutti E,Lucchi F R. Turbidites of the northern Apennines:introduction to facies analysis[J]. International Geology Review,1972,20(2):125-166.
[35] Wu T,Fu Y. Cretaceous deepwater lacustrine dedimentary sequences from the Northernmost South China Block,Qingdao,China[J]. Journal of Earth Science,2014,25(2):241-251.
[36] Roser B P,Cooper R A,Nathan S,et al. Reconnaissance sandstone geochemistry,provenance,and tectonic setting of the lower Paleozoic terranes of the West Coast and Nelson,New Zealand[J]. New Zealand Journal of Geology and Geophysics,1996,39(1):1-16.
[37] Yang R,Fan A,Han Z,et al. A Marine or Continental Nature of the Deltas in the Early Cretaceous Lingshandao Formation——Evidences from Trace Elements[J]. Acta Geologica Sinica,2017,91(1):367-368.
[38] Yang R,Vam L A J. Early Cretaceous slumps and turbidites with peculiar soft-sediment deformation structures on Lingshan Island(Qingdao,China)indicating a tensional tectonic regime[J]. Journal of Asian Earth Sciences,2016.
[39] Yang T,Cao Y,Friis H,et al. Origin and evolution processes of hybrid event beds in the Lower Cretaceous of the Lingshan Island,Eastern China[J]. Australian Journal of Earth Sciences,2018:1-18.
[40]秦雁群,计智锋,万仑坤,等.海相深水碎屑岩层序地层学理论进展及关键问题[J].石油与天然气地质,2017,38(1):12-21.Qin Yanqun,Ji Zhifeng,Wan Lunkun,et al. Theory progress and key issues of deep water marine clastic sequence stratigraphy[J]. Oil&Gas Geology,2017,38(1):12-21.
[41]任拥军,查明.胶莱盆地东北部白垩系烃源岩有机地球化学特征[J].石油大学学报(自然科学版),2003(5):16-20,2.Ren Yongjun,Zha Ming. Organic geochemistry characteristics of cretaceous source rocks in northeast Jiaolai Basin[J]. Journal of China University of Petroleum(Edition of Natural Science),2003(5):16-20,2.
[42]张领军,辛蘶.胶莱盆地水南组页岩有机地球化学特征[J].煤炭与化工,2017,40(1):9-12.Zhang Lingjun,Xin Wei. Organic geochemical characteristics of water group shale in Jiaolan Basin[J]. Coal and Chemical Industry,2017,40(1):9-12.
[43] Saller A,Lin R,Dunham J. Leaves in turbidite sands:The main source of oil and gas in the deep-water Kutei Basin,Indonesia[J].AAPG Bulletin,2006,90(10):1585-1608.
[44] Gastaldo R A,Allen G P,Huc A Y. Detrital peat formation in the tropical Mahakam River delta,Kalimantan,eastern Borneo:Sedimentation,plant composition,and geochemistry[J]. Geological Society of America Special Papers,1993,286:107-118.
[45]李志明,钱门辉,黎茂稳,等.中-低成熟湖相富有机质泥页岩含油性及赋存形式——以渤海湾盆地渤南洼陷罗63井和义21井沙河街组一段为例[J].石油与天然气地质,2017,38(3):448-456.Li Zhiming,Qian Menhui,Li Maowen,et al. Oil content and occurrence in low-medium mature organic-rich lacustrine shales:A case from the 1st member of the Eocene-Oligocene Shahejie Formation in Well Luo-63 and Yi-21,Bonan Subsag,Bohai Bay Basin[J]. Oil&Gas Geology,2017,38(3):448-456.
[46] Moldowan J M,Dahl J,Huizinga B J,et al. The molecular fossil record of oleanane and its relation to angiosperms[J]. Science,1994,265(5173):768-771.
[2]张振凯,周瑶琪,梁文栋,等.山东灵山岛早白垩世构造演化及地质意义[J].海洋地质前沿,2016,32(4):1-10.Zhang Zhenkai,Zhou Yaoqi,Liang Wendong,et al. Early cretaceous tectonic evolution of Lingshan Island in Shandong province and its geologic significance[J]. Marine Geology Frontiers,2016,32(4):1-10.
[3]栾光忠,李安龙,王建,等.青岛主要海岛成因分类及其地质环境分析[J].中国海洋大学学报(自然科学版),2010,40(8):111-116.Luan Guangzhong,Li Anlong,Wang Jian,et al. The geological origin division of the main sea island in Qingdao area and environment analysis[J]. Periodical of Ocean University of China,2010,40(8):111-116.
[4]吕洪波,王俊,张海春.山东灵山岛晚中生代滑塌沉积层的发现及区域构造意义初探[J].地质学报,2011,85(6):938-946.Lu Hongbo,Wang Jun,Zhang Haichun. Discovery of the late mesozoic slump beds in Lingshan Island,Shandong and a pilot research on the regional tectonics[J]. Acta Geologica Sinica,2011,85(6):938-946.
[5]吕洪波,张海春,王俊,等.山东胶南灵山岛晚中生代浊积岩中发现巨大滑积岩块[J].地质论评,2012,58(1):80-81.Lu Hongbo,Zhang Haichun,Wang Jun,et al. Giant landslides found in the Late Mesozoic turbidites in Lingshan Island,Jiaonan,Shandong[J]. Geological Review,2012,58(1):80-81.
[6]梁钊,周瑶琪.山东省灵山岛下白垩统浊积岩中与滑塌作用相关的软沉积物变形构造[J].地球科学,2017,42(10):1715-1724.Liang Zhao,Zhou Yaoqi. Soft sediment deformation structures related to slumping in Lower Cretaceous turbidite in Lingshan Island,Shandong Province[J]. Earth Science,2017,42(10):1715-1724.
[7]王安东,周瑶琪,闫华,等.山东省灵山岛早白垩世软沉积物变形构造特征[J].古地理学报,2013,15(5):717-728.Wang Andong,Zhou Yaoqi,Yan Hua,et al. Characteristics of soft sediment deformation structures of the Early Cretaceous in Lingshan Island of Shandong Province[J]. Journal of Palaeogeography,2013,15(5):717-728.
[8]邵珠福,钟建华,李勇,等.青岛灵山岛晚中生代重力流沉积特征及环境分析[J].地质论评,2014,60(3):555-566.Shao Zhufu,Zhong Jianhua,Li Yong,et al. The sedimentary characteristics and environmental analysis of Late Mesozoic gravity flows in Lingshan Island. Geological Review[J]. 2014,60(3):555-566.
[9]周瑶琪,周腾飞,张振凯,等.山东省灵山岛下白垩统青山群火山地震软沉积物变形构造特征及成因机制[J].古地理学报,2017,19(4):567-582.Zhou Yaoqi,Zhou Tengfei,Zhang Zhenkai,et al. Characteristics and formation mechanism of soft-sediment deformation structures related to volcanic earthquakes of the Lower Cretaceous Qingshan Group in Lingshan Island,Shandong Province[J]. Journal of Palaeogeography,2017,19(4):567-582.
[10] Yang R,Fan A,Han Z,et al. An upward shallowing succession of gravity flow deposits in the Early Cretaceous Lingshandao Formation,Western Yellow Sea[J]. Acta Geologica Sinica,2016,90(4):1553-1554.
[11] Liang Z,Zhou Y,Van L A J. Soft-sediment deformation structures in-duced by rapid sedimentation in Early Cretaceous turbidites,Lingshan Island,eastern China[J]. Canadian Journal of Earth Sciences,2018,55(2):118-129.
[12]于姗姗.山东东部近海晚中生代裂陷盆地沉积相研究[D].东营:中国石油大学(华东),2014.Yu Shanshan. Research on the Sedimentary Facies of Late Mesozoic Rift Basin in the Offshore Area of Eastern Shandong[D]. Dongying:China University of Petroleum(East China),2014.
[13]刘杨.山东近海地区下白垩统沉积岩有机地球化学特征[D].东营:中国石油大学(华东),2014.Liu Yang. Organic geochemical characteristics of Lower Cretaceous sedimentary in the offshore area of Shandong[D]. Dongying:China University of Petroleum(East China),2014.
[14]王安东,周瑶琪,张振凯,等.山东灵山岛莱阳群水下非构造裂缝特征及意义[J].地球学报,2014,35(3):321-328.Wang Andong,Zhou Yaoqi,Zhang Zhenkai,et al. Characteristics and significance of underwater non-tectonic cracks in Laiyang Group of Lingshan Island,Shandong Province[J]. Acta Geoscientica Sinica,2014,35(3):321-328.
[15] Wang J,Chang S C,Lu H B,et al. Detrital zircon U–Pb age constraints on Cretaceous sedimentary rocks of Lingshan Island and implications for tectonic evolution of Eastern Shandong,North China[J]. Journal of Asian Earth Sciences,2014,96:27-45.
[16]张海春,吕洪波,李建国,等.山东青岛早白垩世新地层单位——灵山岛组[J].地层学杂志,2013,37(2):216-222.Zhang Haichun,Lu Hongbo,Li Jianguo,et al. The Ling Shan Dao Formation:a new lithostratigraphic unit of the Early Cretaceous in Qingdao,Shandong,China[J]. Journal of Stratigraphy,2013,37(2):216-222.
[17]吕洪波,张海春,王俊,等.灵山岛早白垩世复理石不是陆内三角洲沉积——答钟建华教授[J].地质论评,2013,59(1):11-14.Lu Hongbo,Zhang Haichun,Wang Jun,et al. The Early Cretaceous Flysch in Lingshan Island is not an intracontinental delta deposit-Answering Professor Zhong Jianhua[J]. Geological Review,2013,59(1):11-14.
[18]钟建华.灵山岛中生代沉积岩是深水远源浊积岩、还是陆内三角洲沉积?——与吕洪波教授商榷[J].地质论评,2012,58(6):1180-1182.Zhong Jianhua. Is the Mesozoic sedimentary rock of Lingshan Island a deep-water distant turbidite or an intra-continental delta?——Discussing with Professor Lu Hongbo[J]. Geological Review,2012,58(6):1180-1182.
[19]邵珠福,钟建华,李勇,等.青岛灵山岛纹层控制的砂级颗粒支撑叠瓦构造的发现及其意义[J].中国科学:地球科学,2014,44(8):1761-1776.Shao Zhufu,Zhong Jianhua,Li Yong,et al. Characteristics and sedimentary processes of lamina-controlled sand-particle imbricate structure in deposits on Lingshan Island,Qingdao,China[J]. Science China:Earth Sciences,2014,44(8):1761-1776.
[20]杨仁超.灵山岛早白垩世重力流沉积类型与沉积环境探讨[C]∥中国地质学会.中国地质学会2015学术年会论文.北京:中国地质学会,2015.Yang Renchao. Discussion on types and sediemntary environment of the Early Cretaceous gravity flow deposits on Lingshan Island[C]∥Geological Society of China Abstract of The 2015 Annual Meeting of Geological Society of China. Beijing:The 2015 Annual Meeting of Geological Society of China,2015.
[21]刘菲菲,周瑶琪,许红,等.灵山岛成因特征、类型及其地质构造意义[J].海洋地质前沿,2016,32(3):33-40.Liu Feifei,Zhou Yaoqi,Xu Hong,et al. Origin of the Lingshan Island and Geotectonic Significance[J]. Marine Geology Frontiers,2016,32(3):33-40.
[22]李守军,张祥玉,赵秀丽,等.山东省青岛市灵山岛下白垩统中发现鱼类和叶肢介化石[J].地质论评,2017,63(1):1-6.Li Shoujun,Zhang Xiangyu,Zhao Xiuli,et al. Discovery of fish and conchostracan fossils in Lower Cretaceous in Lingshan Island,Qingdao,Shandong[J]. Geological Review,2017,63(1):1-6.
[23]张振凯,周瑶琪,彭甜明,等.山东灵山岛莱阳群粉砂岩地球化学特征及意义[J].地球科学,2017,42(3):357-377.Zhang Zhenkai,Zhou Yaoqi,Peng Tianming,et al. Geochemical characteristics and signatures of siltstones from Laiyang Group at Lingshan Island,Qingdao,Shandong[J]. Earth Science,2017,42(3):357-377.
[24]付永涛,虞子冶.青岛垭口—八仙墩变质海相碎屑岩的属性和构造指示意义[J].地质科学,2010,45(1):207-227.Fu Yongtao,Yu Ziye. Attributes and tectonic implications of the metamorphic marine clastic rocks in the Yakou-Baxiandun,Qingdao[J].Chinese Journal of Geology,2010,45(1):207-227.
[25]吴拓宇,赵淑娟,付永涛.青岛八仙墩海相碎屑岩的岩石地球化学特征及其油气研究意义[J].地质科学,2010,45(4):1156-1169.Wu Tuoyu,Zhao Shujuan,Fu Yongtao. Petrogeochemistrical characteristics and its implication for hydrocarbon of the Lower Paleozoic marine siliclastic rocks in Baxiandun,Qingdao[J]. Chinese Journal of Geology,2010,45(4):1156-1169.
[26]王俊.青岛崂山垭口白垩纪海相地层碎屑锆石U-Pb年龄[C]∥中国矿物岩石地球化学学会.中国矿物岩石地球化学学会第14届学术年会论文集,北京:中国矿物岩石地球化学学会,2013:1.Wang Jun. Cretaceous zircon U-Pb age of the Cretaceous marine strata in the Laoshan Yakou,Qingdao.[C]∥Chinese Society for Mine-ralogy,Petrology and Geochemistry. Abstract Paper of the 14th Annual meeting of the Chinese Society for Mineralogy,Petrology and Geochemistry. Beijing:Chinese Society for Mineralogy,2013:1.
[27]赵广涛,王德滋,曹钦臣.崂山花岗岩岩石地球化学与成因[J].高校地质学报,1997(1):2-4,6,9-16.Zhao Guangtao,Wang Dezi,Cao Qinchen. The geochemistry and genesis of the Laoshan granitoids,shandong province[J]. Geological Journal of China Universities,1997(1):2-4,6,9-16.
[28] Wang J,Chang S C,Lin P,et al. Evidence of Early Cretaceous transpression in the Sulu orogenic belt,eastern China[J]. Tectonophysics,2016,687(?):44-55.
[29]张岳桥,李金良,柳宗泉,等.胶莱盆地深部拆离系统及其区域构造意义[J].石油与天然气地质,2006(4):504-511.Zhang Yueqiao,Li Jinliang,Liu Zongquan,et al. Detachment systems in deep of Jiaolai basin and their regional tectonic significance[J].Oil&Gas Geology,2006(4):504-511.
[30]张岳桥,赵越,董树文,等.中国东部及邻区早白垩世裂陷盆地构造演化阶段[J].地学前缘,2004(3):123-133.Zhang Yueqiao,Zhao Yue,Dong Shuwen,et al. Tectonic evolution stages of the Early Cretaceous rift basins in Eastern China and adjacent areas and their geodynamic background[J]. Earth Science Frontiers,2004(3):123-133.
[31] Zhang Y,Dong S,Shi W. Cretaceous deformation history of the middle Tan-Lu fault zone in Shandong Province,eastern China[J]. Tectonophysics,2003,363(3-4):243-258.
[32]张岳桥,董树文,赵越,等.华北侏罗纪大地构造:综评与新认识[J].地质学报,2007(11):1462-1480.Zhang Yueqiao,Dong Shuwen,Zhao Yue,et al. Jurassic tectonics of North China:a Synthetic View[J]. Acta Geologica Sinica,2007(11):1462-1480.
[33]刘华,李凌,吴智平.胶莱盆地烃源岩分布及有机地球化学特征[J].石油实验地质,2006(6):574-580,585.Liu Hua,Li Ling,Wu Zhiping. Distribution and organic geochemical characteristics of hydrocarbon source rocks in the jiaolai basin petroleum[J]. Geology&Experiment,2006(6):574-580,585.
[34] Mutti E,Lucchi F R. Turbidites of the northern Apennines:introduction to facies analysis[J]. International Geology Review,1972,20(2):125-166.
[35] Wu T,Fu Y. Cretaceous deepwater lacustrine dedimentary sequences from the Northernmost South China Block,Qingdao,China[J]. Journal of Earth Science,2014,25(2):241-251.
[36] Roser B P,Cooper R A,Nathan S,et al. Reconnaissance sandstone geochemistry,provenance,and tectonic setting of the lower Paleozoic terranes of the West Coast and Nelson,New Zealand[J]. New Zealand Journal of Geology and Geophysics,1996,39(1):1-16.
[37] Yang R,Fan A,Han Z,et al. A Marine or Continental Nature of the Deltas in the Early Cretaceous Lingshandao Formation——Evidences from Trace Elements[J]. Acta Geologica Sinica,2017,91(1):367-368.
[38] Yang R,Vam L A J. Early Cretaceous slumps and turbidites with peculiar soft-sediment deformation structures on Lingshan Island(Qingdao,China)indicating a tensional tectonic regime[J]. Journal of Asian Earth Sciences,2016.
[39] Yang T,Cao Y,Friis H,et al. Origin and evolution processes of hybrid event beds in the Lower Cretaceous of the Lingshan Island,Eastern China[J]. Australian Journal of Earth Sciences,2018:1-18.
[40]秦雁群,计智锋,万仑坤,等.海相深水碎屑岩层序地层学理论进展及关键问题[J].石油与天然气地质,2017,38(1):12-21.Qin Yanqun,Ji Zhifeng,Wan Lunkun,et al. Theory progress and key issues of deep water marine clastic sequence stratigraphy[J]. Oil&Gas Geology,2017,38(1):12-21.
[41]任拥军,查明.胶莱盆地东北部白垩系烃源岩有机地球化学特征[J].石油大学学报(自然科学版),2003(5):16-20,2.Ren Yongjun,Zha Ming. Organic geochemistry characteristics of cretaceous source rocks in northeast Jiaolai Basin[J]. Journal of China University of Petroleum(Edition of Natural Science),2003(5):16-20,2.
[42]张领军,辛蘶.胶莱盆地水南组页岩有机地球化学特征[J].煤炭与化工,2017,40(1):9-12.Zhang Lingjun,Xin Wei. Organic geochemical characteristics of water group shale in Jiaolan Basin[J]. Coal and Chemical Industry,2017,40(1):9-12.
[43] Saller A,Lin R,Dunham J. Leaves in turbidite sands:The main source of oil and gas in the deep-water Kutei Basin,Indonesia[J].AAPG Bulletin,2006,90(10):1585-1608.
[44] Gastaldo R A,Allen G P,Huc A Y. Detrital peat formation in the tropical Mahakam River delta,Kalimantan,eastern Borneo:Sedimentation,plant composition,and geochemistry[J]. Geological Society of America Special Papers,1993,286:107-118.
[45]李志明,钱门辉,黎茂稳,等.中-低成熟湖相富有机质泥页岩含油性及赋存形式——以渤海湾盆地渤南洼陷罗63井和义21井沙河街组一段为例[J].石油与天然气地质,2017,38(3):448-456.Li Zhiming,Qian Menhui,Li Maowen,et al. Oil content and occurrence in low-medium mature organic-rich lacustrine shales:A case from the 1st member of the Eocene-Oligocene Shahejie Formation in Well Luo-63 and Yi-21,Bonan Subsag,Bohai Bay Basin[J]. Oil&Gas Geology,2017,38(3):448-456.
[46] Moldowan J M,Dahl J,Huizinga B J,et al. The molecular fossil record of oleanane and its relation to angiosperms[J]. Science,1994,265(5173):768-771.
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