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贵阳花溪地区下中三叠统露头层序地层研究
引用本文:时国,田景春,喻美艺.贵阳花溪地区下中三叠统露头层序地层研究[J].沉积与特提斯地质,2010,30(1):11-17.
作者姓名:时国  田景春  喻美艺
作者单位:1. 成都理工大学,沉积地质研究院,四川,成都,610059
2. 贵州大学,资源与环境工程学院,贵州,贵阳,550003
摘    要:贵阳花溪地区下、中三叠统可划分为碳酸盐台地相、台缘相和盆地相三个沉积相区。在对不同相区内典型剖面详细观测、层序界面识别基础上,将下、中三叠统划分为5个Ⅰ型沉积层序和1个Ⅱ型层序。通过研究实测剖面纵向的沉积相变和横向低位岩楔的位置迁移,讨论了区内相对海平面变化。研究区在早-中三叠世经历了一次完整的二级海平面升降旋回:早三叠世与全球海平面变化基本一致,呈上升趋势;中三叠世由于构造作用,海平面总体呈下降趋势,表现出区域特殊性。

关 键 词:层序地层    中三叠统  碳酸盐岩  贵阳

Outcrop sequence stratigraphy of the Middle-Lower Triassic strata in the Huaxi region,Guiyang,Guizhou
SHI Guo,TIAN Jing-chun,YU Mei-yi.Outcrop sequence stratigraphy of the Middle-Lower Triassic strata in the Huaxi region,Guiyang,Guizhou[J].Sedimentary Geology and Tethyan Geology,2010,30(1):11-17.
Authors:SHI Guo  TIAN Jing-chun  YU Mei-yi
Institution:1. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, Sichuan, China; 2. School of Resources and Environmental Engineering, Guizhou University, Guiyang 550003, Guizhou ; China)
Abstract:The Middle -Lower Triassic strata in the Huaxi region, Guiyang, Guizhou are assigned to three sedimentary facies: carbonate platform, platform-margin and basin facies, including five type I and one type II depositional sequences. The study area once experienced a complete second-order cycle of sea-level fluctuation during the Early - Middle Triassic : a rising trend during the Early Triassic and a falling trend due to the effects of regional tectonic movement during the Middle Triassic.
Keywords:sequence stratigraphy  Middle - Lower Triassic  carbonate rock  Guiyang
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