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上下扬子构造演化及叠合盆地油气地质条件对比
引用本文:庞玉茂, 张训华, 肖国林, 温珍河, 郭兴伟, 孙建伟, 赵维娜. 上下扬子构造演化及叠合盆地油气地质条件对比[J]. 海洋地质与第四纪地质, 2016, 36(1): 133-142. doi: 10.3724/SP.J.1140.2016.01013
作者姓名:庞玉茂  张训华  肖国林  温珍河  郭兴伟  孙建伟  赵维娜
作者单位:1. 中国科学院海洋研究所, 青岛 266071;;; 2. 青岛海洋科学与技术国家实验室海洋矿产资源评价与探测技术功能实验室, 青岛 266071;;; 3. 中国地质调查局青岛海洋地质研究所, 青岛 266071;;; 4. 中国海洋大学海洋地球科学学院, 青岛 266100
基金项目:国土资源部海洋地质调查专项(GZH201100202)
摘    要:中国南方海相油气勘探是当前油气勘探的热点领域,并已显示出巨大的勘探潜力。在系统研究扬子块体构造旋回演化及沉积发育的基础上,以地质类比为手段,剖析了上、下扬子区宏观地质特征的异同,认为上、下扬子区叠合盆地演化具有"早期统一、晚期分异"的特征,主要控制因素是扬子块体与周缘构造单元的相互作用,分异的界限大致是以印支运动为界。通过油气地质条件的分析,认为上、下扬子区典型叠合盆地成藏要素存在时空关系上的可类比性,并与构造旋回具有良好的耦合性,在此基础上,重点分析了四川盆地油气勘探对南黄海盆地勘探的指示意义,认为中、古生界海相地层是南黄海油气突破的潜力区,深层油气勘探需重点关注,以及古隆起对油气聚集的关键作用。

关 键 词:扬子块体   南黄海盆地   四川盆地   叠合盆地   构造演化   成藏要素
收稿时间:2015-05-22
修稿时间:2015-12-30

COMPARATIVE STUDY OF TECTONIC EVOLUTION AND PETROLEUM GEOLOGICAL CONDITIONS OF TYPICAL SUPERIMPOSED BASINS IN UPPER AND LOWER YANGTZE BLOCK
PANG Yumao, ZHANG Xunhua, XIAO Guolin, WEN Zhenhe, GUO Xingwei, SUN Jianwei, ZHAO Weina. COMPARATIVE STUDY OF TECTONIC EVOLUTION AND PETROLEUM GEOLOGICAL CONDITIONS OF TYPICAL SUPERIMPOSED BASINS IN UPPER AND LOWER YANGTZE BLOCK[J]. Marine Geology & Quaternary Geology, 2016, 36(1): 133-142. doi: 10.3724/SP.J.1140.2016.01013
Authors:PANG Yumao  ZHANG Xunhua  XIAO Guolin  WEN Zhenhe  GUO Xingwei  SUN Jianwei  ZHAO Weina
Affiliation:1. Institute of Oceanology, Chinese Academy of Science, Qingdao 266071, China;;; 2. Function Laboratory for Marine Mineral Resource Geology and Exploration, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266071, China;;; 3. Qingdao Institute of Marine Geology, China Geological Survey, Qingdao 266071, China;;; 4. Ocean University of China, Qingdao 266100, China
Abstract:The Yangtze region in south China bears great oil potential and is now one of the important sites for petroleum exploration in marine sediments in China. Upon the basis of tectonic evolution and deposition in the Yangtze block, this paper is devoted to the comparative study of the similarities and differences of macro-geological features between the Upper and Lower Yangtzes. The results suggest that the tectonic evolution of the superimposed basins in the upper and lower Yangtze blocks is similar in Paleo-Mesozoic, but different in Meso-Cenozoic. the time boundary of differentiation is about Indosinian and the controlling factors is the interaction among the Yangtze block and adjacent tectonic units. Hydrocarbon accumulation conditions are controlled by basin tectonic evolution and have good coupling pattern with tectonic cycles. The experiences learnt from the Sichuan basin are of great significance to the oil and gas exploration in the South Yellow Sea basin. Upon the fact it is concluded that the Paleo-Mesozoic marine strata is a potential area for break-through of oil and gas exploration in the South Yellow Sea basin. More attention should be paid to the deep strata, and paleo-uplifts are prosperous exploration targets in superimposed basins.
Keywords:Yangtze Block  South Yellow Sea Basin  Sichuan Basin  supeimposed Basin  tectonic evolution  hydrocarbon accumulation elements
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