早三叠世风暴沉积研究进展  

Research Progress on Early Triassic Storm Deposits

作　　者：陈相东 廖纪佳[1] Chen Xiangdong;Liao Jijia(School of Geoscience and Technology,Southwest Petroleum University,Chengdu 610500)

机构地区：[1]西南石油大学地球科学与技术学院,四川成都610500

出　　处：《石化技术》2025年第3期87-89,共3页Petrochemical Industry Technology

摘　　要：风暴沉积的研究对古气候、古地理的恢复和古海洋水动力作用的研究具有重要意义。基于前人对风暴沉积的研究进展,主要从风暴沉积构造、风暴沉积岩石学特征、风暴沉积典型序列和风暴岩与浊积岩之间进行对比,探讨了早三叠世风暴沉积的特点,以期为后续早三叠世风暴沉积的研究提供参考。The study of storm deposits is of significant importance for the restoration of paleoclimate,paleogeography,and the investigation of ancient marine hydrodynamics.Based on previous research on storm deposits,this paper explores the characteristics of early Triassic storm deposits from several aspects,including storm deposit structures,petrographic features of storm deposits,typical storm deposit sequences,and the comparison between storm rocks and turbidite rocks.The aim is to provide reference for the subsequent research on early Triassic storm deposits.

关 键 词：三叠世 风暴沉积 岩相 风暴岩 浊积岩 

分 类 号：P512.2[天文地球—地质学]