沉积与特提斯地质Issue(1)：36-46,11.
鄂尔多斯盆地旬邑地区延长组砂质碎屑流沉积特征及其风暴成因探讨
Sedimentary characteristics and storm origin of the sandy debris flow deposits from the Yanchang Formation in the Xunyi region,Ordos Basin:An approach
摘要
Abstract
The Chang-8 to Chang-6 oil reservoirs from the Yanchang Formation in the southern part of the Ordos Basin belong to the meandering delta-bathyal to abyssal lake deposits with developed gravity flow deposits. These gravity flow deposits were once reported as the turbidity current deposits and sandy debris flow deposits. The latter are supported by the authors on the basis of cores and well logs for the Yanchang Formation in the Xunyi region. These sandy debris flow deposits are originated from the storm processes,and characterized by the storm deposits such as erossional structures,sole casts,wave ripple laminations,wave marks and biological escape traces. The idealized depositional units of storm deposits in the study area consist of the intervals of massive beddings(A),lag deposits(B),parallel beddings( C),hummochy cross-beddings and / or wave ripple laminations( D),and argillutite(E),which are involved into three vertical depositional sequences. The approach to the sandy debris flow deposits and storm processes herein is significant to the study of palaeogeography and palaeoclimates and petroleum exploration in the study area.关键词
旬邑地区/延长组/砂质碎屑流/风暴成因Key words
Xunyi region/Yanchang Formation/sandy debris flow deposits/origin of storms分类
天文与地球科学引用本文复制引用
葛毓柱,钟建华,曲俊利,孙宁亮,王桂林..鄂尔多斯盆地旬邑地区延长组砂质碎屑流沉积特征及其风暴成因探讨[J].沉积与特提斯地质,2014,(1):36-46,11.基金项目
渭北隆起延长组油藏地质特征研究＂项目（ycsy2013ky - A -01）资助 （）
