南盘江盆地中三叠世浊流沉积模式初探

吴应林; 牟传龙

doi:10.11743/ogg19900113

论文 | 浏览量 : 0 下载量: 722 CSCD: 0

PDF
导出
分享
收藏
专辑

南盘江盆地中三叠世浊流沉积模式初探
DISCUSSION ON THE SEDIMENTARY MODEL OF THE MIDDLE TRIASSIC TURBIDITES IN NANPANJIANG BASIN
1990年11卷第1期页码：96-101
网络首发：1990-03-25，

纸质出版：1990
DOI： 10.11743/ogg19900113
稿件说明：

移动端阅览

吴应林, 牟传龙. 南盘江盆地中三叠世浊流沉积模式初探[J]. 石油与天然气地质, 1990,11(1):96-101. DOI： 10.11743/ogg19900113.

Wu Yinglin, Mu Chuanlong. DISCUSSION ON THE SEDIMENTARY MODEL OF THE MIDDLE TRIASSIC TURBIDITES IN NANPANJIANG BASIN[J]. 1990, 11(1): 96-101. DOI： 10.11743/ogg19900113.

摘要

南盘江盆地中三叠世广泛发育一套浊流沉积

为海底扇模式:(1)具一般浊积岩特征;(2)水道沉积明显;(3)浊积岩剖面结构为推进型浊积扇剖面序列。不仅是海底扇

面且是多物源、多个浊积扇的堆积体。

Abstract

Turbidity current deposits were developed widely in Nanpanjiang Basin during the Middle Trias-sic.The sedimentary model is submarine fan.This is based mainly on that:1.They have the character-istics of turbidity current deposits.2.They have obvious channel deposits.3.The sequences of the tur-bidity are prograding turbidite fan in the texture profile.The sedimentary model of the turbidity current deposits in the area is not only submarine fan

but several fans with multi-source.