...
首页> 外文期刊>Carbonates And Evaporites >General depositional features of the carbonate platform gas reservoir of the Lower Triassic Jialingjiang Formation in the Sichuan Basin of southwest China: Moxi gas field of the central basin
【24h】

General depositional features of the carbonate platform gas reservoir of the Lower Triassic Jialingjiang Formation in the Sichuan Basin of southwest China: Moxi gas field of the central basin

机译:西南四川盆地下三叠统嘉陵江组碳酸盐台地气藏总体沉积特征:中部盆地磨溪气田

获取原文
获取原文并翻译 | 示例
           

摘要

The Lower Triassic Jialingjiang Formation gas reservoir in Sichuan Basin of southwest China is a representative carbonate platform reservoir. However, it has not been well studied due to relatively less production in comparison with the reservoir in the well-known underlying Upper Permian Changxing and Lower Triassic Feixianguan formations. Thus, to provide supplement to the hot study of carbonate platform reservoirs in the Sichuan Basin, the authors describe the general depositional features of the carbonate platform gas reservoir of the Jialingjiang Formation based on a case study of the representative second member of the formation (termed as Jia 2) in the Moxi gas field of the central basin. The features mainly include depositional setting, lithology, depositional structure, depositional sequence and reservoir space. These results lead to a conclusion that the Jialingjiang Formation reservoir (the second member in particular) is not of a tidal flat deposition in an intertidal (to supratidal) environment as previously suggested but of restricted and evaporative carbonate platform deposition in a subtidal environment. The tidal flat-like (i.e., platform flat) facies occur only in the Jia 2~2-B layer. Moreover, the restricted-evaporative carbonate platform facies can be further divided into 5 subfacies and 23 microfacies, of which the facies of grain shoal and dolomitic flat are relatively favorable for the development of reservoirs. Their depositional model, distribution and evolution were further tentatively suggested. The facies are subject to paleotomography and sea level variations. These results also have general implications for the carbonate platform reservoirs elsewhere.
机译:中国西南地区四川盆地下三叠统嘉陵江组气藏是典型的碳酸盐台地层。但是,由于与知名的下二叠统长兴组和下三叠统飞仙关组的储层相比产量相对较少,因此尚未进行很好的研究。因此,为补充四川盆地碳酸盐台地层储层的热力研究成果,作者以典型的嘉陵江组第二段为例,描述了嘉陵江组碳酸盐台地气藏的一般沉积特征。如贾2)在中部盆地磨溪气田。这些特征主要包括沉积背景,岩性,沉积结构,沉积层序和储层空间。这些结果得出的结论是,嘉陵江组储层(特别是第二个储层)在潮间(至潮间带)环境中不是潮滩沉积,而是在潮下环境中是受限制的蒸发碳酸盐台地沉积。滩涂状(即平台状)相仅出现在贾2〜2-B层中。此外,限蒸发碳酸盐台地相又可以分为5个亚相和23个微相,其中,浅滩相和白云质相的相较有利于储层的发育。初步提出了它们的沉积模型,分布和演化。这些相易受古断层和海平面变化的影响。这些结果对其他地方的碳酸盐台地油藏也具有普遍意义。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号