摘要
陕西富平地区上奥陶统赵老峪组发育等深流沉积。以实测剖面、岩石光面、薄片资料以及地球化学资料为基础,结合前人研究成果,对赵老峪组等深积岩类型、层序以及等深流沉积发育的影响因素进行了分析。研究认为:(1)赵老峪组发育灰泥等深积岩和粉屑等深积岩2种类型,识别出由单一的灰泥等深积岩以及灰泥等深积岩与粉屑等深积岩组成的2种等深积岩层序;(2)等深流水团温度越低,盐度越高,则等深流强度越大;(3)等深流水团水温由高变低、再变高,盐度由低变高、再变低,可能造成了等深积岩层序由细变粗、再变细;(4)古水深变大、古气候变干热、古盐度变低有利于等深流和等深流沉积的发育。
The Upper Ordovician Zhaolaoyu Formation in Fuping area of Shaanxi Province developed contour current deposits. On the basis of the section measured in field survey,the smooth surface rock,rock thin sections and geochemical data,integrated with previous researches,the authors carried out detailed studies of the types of contourites,the contourite sequences and the influencing factors of contour current deposits. The results show that： （1）The contourites can be classified into two types,i.e. the calcilutitic contourite and the calcisiltitic contourite, and two types of contourite sequences were identified,a single contourite sequence and a calcisiltitic-calcilutitic contourite sequence;（2）As the temperature of contour current water mass gets lower and the salinity gets higher,the contour current strength becomes greater;（3）When the temperature of contour current water mass changes from high to low,then to high, and the salinity of the contour current water mass changes from low to high,then to low, the contourite sequences changes from fine to coarse and then to fine;（4）Larger palaeowater depth,drier and hotter paleoclimate,and lower paleosalinity were favorable for the development of contour current and contour current deposits.
出处
《古地理学报》
CAS
CSCD
北大核心
2017年第1期161-174,共14页
Journal of Palaeogeography：Chinese Edition
基金
国家自然科学基金项目(批准号:41472096)资助~~
关键词
等深流
等深积岩
等深积岩层序
富平地区
上奥陶统
赵老峪组
contour current
contourite
contourite sequence
Fuping area
Upper Ordovician
Zhaolaoyu Formation
作者简介
黄伟，男，1989年生，硕士研究生，矿产普查与勘探专业。E—mail：hw1204740478@163.com
通讯作者简介 何幼斌，男，1964年生，教授，主要从事沉积学的教学与研究。E-mail：heyoubjn@yangtxeu.edu.cn
