WANG Zhenliang and CHEN Heli
, 2002, 29(3): 196-0.
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On the basis of distribution and evolution of paleo-hydrodynamic influencing hydrocarbon migration and accumulation, it is set forth about periods, scopes of expulsion from source rocks, directions of secondary migration and the distribution of profitable convergence areas in reservoir rocks, and the history of accumulation and pooling in Taibei depression is analyzed and summarized. It is discovered, the main periods of expulsion in coal-measure source rocks of lower and middle Jurassic series is early Cretaceous epoch and Pliocene up to now respectively, and the high efficiency of expulsion in middle and eastern areas is developed during early Cretaceous epoch, in contrast, in middle and western areas is Pliocene up to now. The distribution and evolution of fluid potential is of succession. By the way, the relatively low potential areas among high potential areas and those parts located in periphery of high potential areas are directions of secondary migration, and the former is divided into three types—most profitable, profitable and fairly profitable, based on the conditions of migration and accumulation. According to the history of hydrocarbon generation and expulsion, evolution of fluid pressure and fluid potential, the behavior of hydrocarbon in Jurassic system is divided into two major phases of accumulation and pooling in Taibei depression, i.e. phase of early Cretaceaous epoch and Quaternary Period respectively. During the first accumulation stage, the behavior of hydrocarbon is mainly occurred in middle and eastern part of the depression, and the directions of secondary migration and most profitable accumulation areas are Xiaocaohu, Qiudong and their adjacent areas, where at second accumulation stage, active accumulation is mainly developed on middle and western part, and the former existed oil and gas pool is to be remold and complement to some extent.