甘肃及邻近地区第三纪地层概要
AN OUTLINE OF THE TERTIARY STRATIGRAPHY OF GANSU PROVINCE AND ITS NEIGHBOURING AREAS
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摘要: 甘肃及邻近地区的第三系均为陆相湖盆及山间凹地型沉积,它们在各地的分布和发育程度完全受当时沉积环境的控制。较大型的沉积盆地主要分布于祁连山北麓及甘肃东部,而北山、祁连山、秦岭三个地区则沿断陷分布着一些规模不等的山间沉积凹地。二十世纪三十年代以来,不少中、外地质及古生物工作者曾对本地区的第三系进行考察,特别是1958年以来,通过区域地质调查及其他研究工作,积累了很多宝贵资料,但由于以往各研究者的工作范围、工作时间、工作性质和深度不同,所以在地层划分、时代归属等方面长期没有得到统一,因而也造成地层对比的混乱。近年来,在进行断代地层总结的过程中,我们发现以往所厘定的一些下第三系有不少应依据新发现的古生物资料及区域地层对比划归上白Abstract: The Tertiary System in Gansu and its neighbouring areas consists all of sediments of continental lake basin and intermontane depression types. As there existed many problems on the stratigraphic division and age assignment in the past, confusion arose in respect to the stratigraphic correlation. On the basis of the paleontologic data combined with the depositional character- istics, rock associations, ore potentiality and contact relationships, this paper proposes a rational scheme of stratigraphic division and correlation and sum- marizes the stratigrphic features and ancient biotas of various sedimentary basins.