山东东部白垩系莱阳群沉积地层与有机质特征

doi:10.11743/ogg20190111

石油与天然气地质 ›› 2019, Vol. 40 ›› Issue (1): 109-122.doi: 10.11743/ogg20190111

山东东部白垩系莱阳群沉积地层与有机质特征

周瑶琪^1,2,3, 辜洋建^1,2,3, 周腾飞^1,2,3, 岳会雯⁴, 李曼洁^1,2,3, 尹兴城^1,2,3, 梁钊^1,2,3, 曹梦春^1,2,3, 董诗绘^1,2,3

1. 中国石油大学(华东) 地球科学与技术学院, 山东青岛 266580;
2. 海洋国家实验室海洋矿产资源评价与探测技术功能实验室, 山东青岛 266071;
3. 深地资源勘查理论与技术协同创新中心, 山东青岛 266580;
4. 德国波茨坦地学研究中心, 德国波茨坦 D-14473

收稿日期:2018-09-13 修回日期:2018-10-10 出版日期:2019-02-28 发布日期:2018-12-08
作者简介:周瑶琪(1963-),男,博士,教授,博士生导师,地球化学及盆地动力学。E-mail:zhouyq@upc.edu.cn。
基金资助:
国家自然科基金项目（GZH201200510）；山东省重大科技创新工程项目（2017CXGC1608）；十三五科技部基础项目（2017FY201407-1）。

Sedimentary strata and organic matter features of the Cretaceous Laiyang Group in eastern Shandong Province

Zhou Yaoqi^1,2,3, Gu Yangjian^1,2,3, Zhou Tengfei^1,2,3, Yue Huiwen⁴, Li Manjie^1,2,3, Yin Xingcheng^1,2,3, Liang Zhao^1,2,3, Cao Mengchun^1,2,3, Dong Shihui^1,2,3

1. School of Geosciences, China University of Petroleum(East China), Qingdao, Shandong 266580, China;
2. Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao, Shandong 266071, China;
3. Collaborative Innovation Center for Deep Resources Exploration Theory and Technology, Qingdao, Shandong 266580, China;
4. GFZ German Research Centre for Geoscience, Section 3.2 Organic Geochemistry, D-14473 Potsdam, Germany

Received:2018-09-13 Revised:2018-10-10 Online:2019-02-28 Published:2018-12-08

摘要/Abstract

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（Ⅱ₁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。

关键词: 有机质特征, 沉积地层, 莱阳群, 胶莱盆地, 山东东部

Abstract:

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 Ⅱ₁),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 Ⅱ₁)types in high to over mature stage,and the turbidites of Lingshan Island may have completed the process of hydrocarbon generation and expulsion.

Key words: organic feature, sedimentary stratum, Laiyang Group, Jiaolai Basin, eastern Shandong Province

中图分类号:

TE122.1

周瑶琪,辜洋建,周腾飞,等. 山东东部白垩系莱阳群沉积地层与有机质特征[J]. 石油与天然气地质, 2019, 40(1): 109-122. doi: 10.11743/ogg20190111 Zhou Yaoqi,Gu Yangjian,Zhou Tengfei,et al. Sedimentary strata and organic matter features of the Cretaceous Laiyang Group in eastern Shandong Province[J]. Oil & Gas Geology, 2019, 40(1): 109-122. doi: 10.11743/ogg20190111

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山东东部白垩系莱阳群沉积地层与有机质特征

Sedimentary strata and organic matter features of the Cretaceous Laiyang Group in eastern Shandong Province

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