柴北缘西段新近系上干柴沟组沉积相特征分析

详细信息

Sedimentary facies in the Neogene Upper Ganchaigou Formation on the northern margin of the Qaidam Basin, Qinghai

1. Liwu Copper Mining Co., Ltd., Garze Chengdu 610091), Sichuan, China;
2. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, Sichuan, China

摘要: 根据野外露头、岩心观察及录井、测井资料,研究了柴北缘西段新近系上干柴沟组沉积相类型和沉积特征。结果表明:上干柴沟组发育冲积扇、扇三角洲、辫状河、辫状河三角洲、湖泊及颗粒流等六种沉积相类型,其中在鄂博梁-冷湖-潜西发育了一套扇三角洲-湖泊沉积体系,在马海-南八仙地区发育冲积扇-辫状河-辫状河三角洲-湖泊沉积体系。
- 沉积相 /
- 沉积相模式 /
- 上干柴沟组 /
- 柴达木盆地
Abstract: The examination of the sedimentary facies is based on the field outcrops, core observation and well logs for the Neogene Upper Ganchaigou Formation on the northern margin of the Qaidam Basin, Qinghai. The Upper Ganchaigou Formation is built up of the alluvial fan, fan delta, braided stream, braided delta, lacustrine facies and grain flow deposits. Two depositional systems have been recognized, including the fan delta-lacustrine depositional system in the Eboliang-Lenghu-Qianxi zone, and alluvial fan-braided stream-braided delta-lacustrine depositional system in the Mahai-Nanbaxian zone. The results of research in the western part of the northern margin of the Qaidam Basin may provide reliable geological information for further petroleum exploration.
- sedimentary facies /
- sedimentary facies model /
- Upper Ganchaigou Formation /
- Qaidam Basin