首页> 外文期刊>Scientia geologica sinica >Sedimentary characters and Depositional models of the upper Sha-Ⅲ member of the oligocene Shahejie formation in the central Uplift zone, Huimin depression, China
【24h】

Sedimentary characters and Depositional models of the upper Sha-Ⅲ member of the oligocene Shahejie formation in the central Uplift zone, Huimin depression, China

机译:中国惠民凹陷隆起区中新统沙河街组上沙三段上段的沉积特征和沉积模式

获取原文
获取原文并翻译 | 示例
       

摘要

This paper deals with the sedimentology and depositional model for a shore to shallow lake shoal, which developed during the upper Sha-Ⅲ Member of the Oligocene Shahejie Formation (abbreviated as Es3u) according to analyses of core, thin sections, heavy minerals, well-logging and seismic reflections. Five microfacies, i.e., fore-shoal, outer shoal edge, shoal core, inner shoal edge, and back-shoal, have been regognized in this shore to shallow lake shoal. The sandbody and its petrophysics are the best with respect to reservoir property. The shoal depositional environment was associated with storm deposits.
机译:本文通过对岩心,薄层,重矿物,井眼,岩心,薄层,重矿物,岩浆,岩心,岩心,岩心,岩心,岩心,岩心,岩心,岩心,岩心,岩心,岩心,岩心,岩心和沉积物的沉积过程进行了研究。测井和地震反射。在这条海岸至浅湖浅滩中已识别出五个微相,即前浅滩,浅滩外边缘,浅滩核心,浅滩内边缘和后浅滩。就储层性质而言,砂体及其岩石物理学是最好的。浅滩沉积环境与暴风雨沉积有关。

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