塔里木盆地轮古东地区前石炭纪古岩溶微地貌及岩溶发育模式  

Micro-Paleogeomorphology and Karst Development Model of the Pre-Carboniferous in Eastern Lungu Area,Tarim Basin

作　　者：张庆玉[1,2] 梁彬[2] 曹建文[1,2] 淡永[2] 李景瑞[2] 陈利新[3] 

机构地区：[1]中国地质大学(武汉)环境学院 [2]中国地质科学院岩溶地质研究所/国土资源部岩溶动力学重点实验室 [3]中国石油塔里木油田分公司勘探开发研究院

出　　处：《海相油气地质》2017年第3期30-36,共7页Marine Origin Petroleum Geology

基　　金：国家自然科学基金"塔里木盆地高温高压奥陶系碳酸盐岩溶蚀机理研究"(41302122);国家"973计划"项目课题"地表和近地表条件下岩溶缝洞充填过程及机理研究"(2011CB201001);国土资源部公益性行业科研专项"塔里木古潜山奥陶系风化壳油藏岩溶储层预测"(201211082);中国地质调查局项目"红水河上游岩溶流域1:5万水文地质环境地质调查"(DD20160300)共同资助

摘　　要：以现代岩溶理论为指导,应用"印模与残厚组合法"恢复岩溶古地貌,在4种二级地貌类型(岩溶高地、岩溶陡坡地、岩溶缓坡地和岩溶盆地)划分的基础上,将塔里木盆地轮古东地区前石炭纪古岩溶地貌进一步划分为峰丛洼地、丘峰谷地、溶丘洼地、峰丛垄脊沟谷、峰丘洼地、丘丛垄脊沟谷、岩溶谷地、溶丘平原等8种三级地貌类型。并在垂向岩溶分带研究的基础上,明确了不同古岩溶地貌条件下的岩溶发育特征及充填机制。研究认为:岩溶高地为区域补给区,发育溶蚀裂缝和溶洞系统;岩溶陡坡地为补给-径流区,以高角度溶蚀裂缝为主;岩溶缓坡地为地下水径流区,发育暗河管道系统;岩溶盆地为排泄区,岩溶缝洞充填程度高。Guided by modern karst theory,the paleogeomorphology of the pre-Carboniferous Eastern Lungu area in Tarim Basin was restored by using the combination of impression method and residual method.Based on the identification of 2nd-grade geomorphological units including four types as karst upland,karst steep slope,karst gentle slope and karst basin,3rd-grade geomorphological units are further divided,including eight types as peak cluster depression,Qiu Feng valley,karst dome-depression,peak cluster ridge in valleys,peak hill depressions,Qiu Cong ridge in valleys,karst valley,karst dome-plains.Through the study of vertical paleokarst zoning,the development characteristics and filling mechanism of karst in different paleolandform units were definite.It is concluded that the karst highland is a recharge area in which developed karst crack and cave system; karst steep slope is a recharge and runoff area in which developed high angle corrosion cracks; karst gentle slope is a groundwater runoff area in which developed underground river pipeline system; karst basin is a discharge area in which developed fissure and hole system with highly filling.

关 键 词：古地貌 古岩溶 轮南古潜山 碳酸盐岩 奥陶纪 塔里木盆地 

分 类 号：TE121.31[石油与天然气工程—油气勘探] TE122.23