越南北宋红盆地前新生代碳酸盐岩岩石学和生物地层特征

Mai Hoang Dam, N. T. Trieu, Lieu Kim Phuong
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摘要

越南宋红盆地北部前新生代碳酸盐岩是石油公司勘探开发中考虑和研究的对象。这些岩石中已发现油气成藏,具有显著的商业储量,其中孔隙度对油气容量的估计起着重要作用。碳酸盐岩主要由结晶灰岩、包覆岩、微晶岩和泥岩组成,经历了白云化、压实和溶蚀作用。碳酸盐岩孔隙系统主要有裂缝型、孔洞型和晶间型。大型底栖有孔虫组合的优势表明,碳酸盐沉积形成于晚古生代(石炭-二叠纪),沉积于浅海环境。此外,所获得的岩石学和生物地层特征与邻近卡特巴岛地区暴露的碳酸盐地层具有良好的相关性。研究结果可用于越南北部的石油勘探或局部地层对比。
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Petrological and Biostratigraphic Characteristics of Pre-Cenozoic Carbonate Rocks in the Northern Song Hong Basin, Vietnam
Pre-Cenozoic carbonate rocks in the northern Song Hong basin, Vietnam that are being considered and studied by oil companies in exploration and exploitation. The hydrocarbon accumulations in these rocks have been discovered and have significantly commercial reserves, in which the porosity plays an important role in estimating the capacity of hydrocarbon. The carbonate rocks are composed mainly of crystalline limestone, packstone, wackestone and mudstone, which have been experienced dolomitization, compaction and dissolution. The main carbonate pore systems include fracture, vuggy and intercrystalline porosity. The predominance of larger benthic foraminiferal assemblages indicates that the carbonate sediments were formed during the late Paleozoic (Carboniferous-Permian) and were deposited in shallow marine environment. Furthermore, the obtained petrological and biostratigraphic characteristics are well-correlated with the carbonate formations exposed in adjacent Cat Ba island area. The results of this study are either used in petroleum exploration or used in a local stratigraphic correlation in northern Vietnam.
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