合肥侏罗纪盆地性质及其与大别造山带沉积响应  

CHARACTERISTICS OF THE HEFEI JURASSIC BASIN AND ITS SEDIMENTARY RESPONSE TO THE DABIESHAN OROGENIC BELT

作　　者：王亚琳[1] 杨贵丽[2] 徐春华[3] 

机构地区：[1]中国科学院广州地球化学研究所,广州510640 [2]中国石油化工股份有限公司胜利油田分公司地质科学研究院,山东东营257015 [3]中国石油化工股份有限公司胜利油田分公司勘探项目管理部,山东东营257000

出　　处：《石油实验地质》2007年第1期57-62,共6页Petroleum Geology & Experiment

基　　金：国家自然科学基金项目(40272094)

摘　　要：从盆—山耦合关系角度研究大别造山带与合肥侏罗纪盆地的性质,提出伴随着大别山的第二次隆升,早侏罗世大别山北缘出现了最强的沉降—沉积,形成了合肥侏罗纪前陆盆地;随后中—晚侏罗世时盆地南部沉降—沉积强度显示出变弱的趋势,期间没有再出现沉降—沉积再加强的现象。简要介绍了盆地不同地区侏罗纪地层的沉积物特征及发育特点,在此基础上,从盆地结构、沉积物碎屑骨架组分、层序结构、沉积体系等角度研究了合肥侏罗纪盆地对大别造山带的响应,指出二者之间具有较好的耦合关系。Characteristics of the Hefei Jurassic Basin and the Dabieshan Orogenic Belt have been studied from the aspect of basin-and-range coupling in this paper. With the second uplifting of the Dabieshan Mountain, the northern fringe of the Dabieshan Mountain underwent the strongest subsidence and sedimentation in the early Jurassic and then the Hefei Jurassic Foreland Basin was formed. Afterwards, the subsidence-sedimentation process slowed clown gradually in the south of the Hefei Basin in the Middle-Late Jurassic without any strengthening phenomenon. The authors also briefly introduce the sediment characteristics of the Jurassic Formation in different areas of the Hefei Basin. On this basis, the sedimentary response to the Dabieshan Orogenic Belt of the Hefei Jurassic Basin is studied thoroughly from the aspects of basin structure, clastic matrix constituents of sediments, sequence architecture and sedimentary system, and so on. The study demonstrates that these two things are coupling very well.

关 键 词：沉积响应 结构响应 盆地格架 层序格架 侏罗纪盆地性质 合肥盆地 

分 类 号：TE121.2[石油与天然气工程—油气勘探]