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六盘山地区白垩纪沉积盆地层序地层及盆地演化动力学分析
引用本文:周玲琦,仲新,张有龙.六盘山地区白垩纪沉积盆地层序地层及盆地演化动力学分析[J].甘肃地质学报,2005,14(2):43-52.
作者姓名:周玲琦  仲新  张有龙
作者单位:甘肃省地矿局第三地勘院,甘肃,兰州,730050;中国地震局兰州地震研究所,甘肃,兰州,730000
摘    要:六盘山白垩纪盆地是六盘山内陆叠合盆地的一个单型盆地。形成了冲积扇—扇三角洲—滨浅湖泊、三角洲前缘—滨浅湖—中深湖、中深湖—浅湖沉积体系组合型式。充填序列划分为一个Ⅱ级及五个Ⅲ级构造层序,分别对应于初始裂陷、扩张裂陷—稳定坳陷、湖盆萎缩整体抬升3个演化阶段。

关 键 词:六盘山地区  白垩纪盆地  层序  动力学分析
文章编号:1004-4116(2005)02-0043-0010
收稿时间:2005

ANALYSIS OF STRATA AND BASIN EVOLUTION DYNAMICS OF CRETACEOUS SEDIMENTARY BASIN SEQUENCE IN LIUPAN MOUNTAINOUS AREA
ZHOU Ling-qi,ZHONG Xin and ZHANG You-long.ANALYSIS OF STRATA AND BASIN EVOLUTION DYNAMICS OF CRETACEOUS SEDIMENTARY BASIN SEQUENCE IN LIUPAN MOUNTAINOUS AREA[J].Acta Geologica Gansu,2005,14(2):43-52.
Authors:ZHOU Ling-qi  ZHONG Xin and ZHANG You-long
Institution:1. No. 3 Geology and Mineral Exploration Team, Gansu Provincial Bureau of Geology and Mineral Exploration and Development, Lanzhou 730050, China ; 2. Lanzhou Institute of Earthquake, China Earthquake Administration, Lanzhou 730020, China
Abstract:Liupanshan Cretaceous basin is a mono - basin of Liupanshan inland overlapping basin. It formed such association types as alluvial fan - fan delta - shallow coastal lake, delta front - shallow coastal lake- semi - deep lake, semi- deep lake shallow lake sedimentary system. Filling sequences are divided one II class structural sequence, and five III class structural sequences, which belong to 3 evolution stages of initial depression, spreading depression stable depression, lake basin reducing accordingly.
Keywords:Liupan mountainousarea  Cretaceous basin  Sequence  Dynamic analysis
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