摘要
深水牵引流沉积主要分为等深流沉积和内波内潮汐沉积两类。前者可形成巨大的堆积体——等深积岩丘,其规模可与海底扇相比拟。现代海洋大陆坡及陆隆地带等深积岩丘非常发育;古代地层记录中也有等深积岩丘,如已开采数十年的阿拉伯克拉通白垩系等深积岩丘油田。后者则不仅可形成分选极好的砂级沉积物,而且可形成规模巨大的“沉积物波”,并成群成带地出现。海洋中沉积物波的迁移可形成巨大的沉积体。在世界各大洋深盆海底,均有大范围分布的现代大型沉积物波。中国地层记录中的大型沉积物波,首先在塔里木盆地塔中地区中一上奥陶统中被识别出来,并有良好油气显示。认为中国的广大地区发育有多个时代的海相深水沉积,深水牵引流沉积储集层是中国21世纪油气勘探具巨大潜力和现实可行性的新领域。其油气勘探首选地区是塔里木盆地、扬子地台南缘和鄂尔多斯西缘。
Deep-water traction current deposits mainly include contour current deposits and internal-wave/internal-tide deposits.The former can form giant sedimentary bodies,the contourite drifts,which are comparable to large submarine fans in extent. Contourite drifts are well-developed along modern continental slopes and rises.The ancient contourite drifts in the strati- graphic record were reported in literatures,such as the Creta- ceous contourite drift on the continental margin of Arabian Cra- ton,a huge oil field that have been produced for several decades.The latter can not only form well-sorted sand-size deposits but also large-scale sediment waves occurred in groups.The sediment waves migrated in oceans can bring in a large-soale sedimentary body.There are large-scaled modern sediment waves wide-distributed on the deep-sea floors of the every ocean basin.A large-scaled sediment wave reservoir in stratigraphic record,which has good oil shows,was first rec- ognized in the Middle-Upper Ordovician strata in Tarim Basin. Deep-water marine deposits were well-developed in the vast areas of China in many geological times so that the reservoirs of deep-water traction current deposits should be a new greatly potential field for China's petroleum exploration in 21 century. The preferred regions should include Tarim Basin,south margin of Yangtze Platform and west margin of Ordos Basin.
出处
《海相油气地质》
2002年第4期1-7,共7页
Marine Origin Petroleum Geology
基金
国家自然科学基金(批准号:40272060)
关键词
深水牵引流沉积
等深流沉积
内波沉积
内潮汐沉积
油气藏
油气勘探
中国
Deep-water traction
Contourite deposit
Internalwave deposit
Internal-tide deposits
Contourite drift reservoir
Oil and gas exploration
China