[an error occurred while processing this directive] 世界地质 2018, 37(4) 1085-1091 DOI:     ISSN: 1004-5589 CN: 22-1111/P

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本文关键词相关文章
辽北地区
殷屯组
陈千户组
汎河组
二次冰期
间冰期
本文作者相关文章
卢崇海
田德欣
李彪
邵九龙
刘振伟
赵娇
卢思桥
PubMed
Article by Lu C
Article by Tian D
Article by Li B
Article by Shao J
Article by Liu Z
Article by Zhao J
Article by Lu S
辽北地区新元古代原殷屯组岩石地层单位的重新划分及其地质意义
卢崇海,田德欣,李彪,邵九龙,刘振伟,赵娇,卢思桥
1. 辽宁省矿产勘查院,沈阳 110031; 2. 辽宁省地质矿产研究院,沈阳 110032
摘要

本次研究把 20 世纪八十年代初期完成的辽宁 1∶ 5 万大甸子、下肥地和上年马洲幅区调报告中 所建立的震旦系殷屯组 3 个岩性段,即底部砾岩段、中部砂岩段和上部板岩、页岩段,分别厘定为新 元古界北方系 ( 南华系) 殷屯组、陈千户组和汎河组。并确认出殷屯组为辽宁北方系 ( 南华系) 第 一次陆相冰碛作用的产物; 陈千户组为陆相间冰期沉积的产物; 汎河组为辽宁第二次陆相冰湖相堆积 的产物。上述组级岩石地层单位的厘定,首次在辽宁北部地区划分出 2 次冰水堆积物。

关键词 辽北地区   殷屯组   陈千户组   汎河组   二次冰期   间冰期  
Re-division of lithostratigraphic units of previous Neoproterozoic Yintun Formation and its geological significance in northern Liaoning
LU Chong-hai,TIAN De-xin,LI Biao,SHAO Jiu-long,LIU Zhen-wei,ZHAO Jiao,LU Si-qiao
1. Liaoning Institute of Mineral Exploration,Shenyang 110031,China; 2. Liaoning Institute of Geology and Mineral Resources,Shenyang 110032,China
Abstract: Sinian Yintun Formation was originally established during the 1∶ 50 000 regional geological survey in Dadianzi,Xiafeidi and Shangnianmazhou area in the early eighties of 20 century. In this study,the authors rede- fined the previous three lithologic units of Yintun Formation as Yintun,Chenqianhu and Fanhe formations of Neo- proterozoic Beifang System (Nahua System). Meanwhile,it is confirmed that Yintun Formation was the product of the first continental moraine in Beifang System (Nahua System) in Liaoning,Chenqianhu Formation was the prod- uct of continental interglacial deposition,and Fanhe Formation was the product of the second continental glacial la- custrine deposit in Liaoning. It is the first time to determine two ice-water deposits in northern Liaoning.
Keywords: northern Liaoning   Yintun Formation   Chenqianhu Formation   Fanhe Formation   twice ice age   interglacial period  
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1.田德欣, 卢崇海, 蔡新明, 王彬娜, 徐耸, 王强, 卢思桥.辽南新元古代桥头组海相冰碛沉积事件[J]. 世界地质, 2018,37(4): 1092-1100

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