北京地区新生界研究史  

RESEARCH HISTORY OF CENOZOIC ERATHEM,BEIJING

作　　者：吕金波[1] 李伟[2] 

机构地区：[1]北京市地质调查所,102206 [2]北京市地质矿产局,100050

出　　处：《北京地质》2000年第1期1-7,共7页Beijing Geology

摘　　要：北京的新生界研究始于 1 91 8年 ,研究程度较高 ,成因类型齐全 ,主要有洪水形成的长辛店组、洞穴碎屑堆积的鱼岭组和周口店组、风成的马兰黄土、泥炭成因的肖家河组和尹各庄组、海相层、冰碛层以及岩熔洞穴中的次生化学沉积物等。Started in 1918,the research on cenozoic erathem in Beijing has already reached a deeper level.Varieties of sediments have been found here,mainly including Ghangxingdian Formation formed by flood,Yuling and Zoukoudian Formation as cave detritus sediments,Malan loess as a kind of eolian deposit,Xiaojiahe and Yinggezhuang Formation originated from peat.Marine sediment,till sheet and spelothem.

关 键 词：研究史 新生界 北京 地层 历史地质 

分 类 号：P534.6[天文地球—古生物学与地层学]