首页|库车坳陷上三叠统黄山街组沉积特征及地质意义

库车坳陷上三叠统黄山街组沉积特征及地质意义

扫码查看
塔里木盆地库车坳陷三叠系黄山街组为一套源、储、盖共生的地层,是未来潜在的油气勘探目标。但目前缺乏其详细沉积特征与演化方面的研究,不利于对古地理演化的理解。故基于多条露头剖面,详细分析沉积特征并揭示其地质意义,结果表明:①黄山街组一段与二段构成向上变深的下旋回,三段构成向上变深但不完整的中旋回,四段构成浅→深→浅的上旋回;②由砾质粗碎屑构成的黄山街组一段与三段是物源区在印支运动中两幕强烈隆升的沉积响应;③黄山街组中发育有洪水、地震等所致的事件沉积;④黄四段发育的暗色泥岩是高可容纳空间下充足物源的快速沉积;⑤黄三段沉积之后发生了区域性的构造抬升及构造—沉积转换,源区也呈准平原化;⑥黄四段与下伏黄三段及上覆塔里奇克组之间均存在一定的沉积间断。
Sedimentary characteristics and geological significance of Upper Triassic Huangshanjie Formation in Kuqa Depression
Objectives:The Upper Triassic Huangshanjie Formation in the Kuqa depression,Tarim Basin,is a set of strata with source,reservoir and cap coexistence,which is a potential target of oil and gas exploration in the future.However,at present there is a lack of detailed research on its sedimentary characteristics,which is not conducive to understanding the evolution of paleogeography.Methods:Based on careful observation of the sedimentary phenomena on the multiple outcrop sections,the sedimentary characteristics were analyzed in detail and the revealed geological significance were studied.Results:①In Huangshanjie Formation,the deep-up lower cycle is formed with the First and Second Members,the incomplete deep-up middle cycle is formed with the Third Member,and the upper cycle changing from shallow→ deep → shallow is formed with the Fourth Member;② the First and Third Members of the Huangshanjie Formation,formed with pebbly coarse clasts,are the sedimentary responses to two episodes of intense uplift in the provenance area during the Indosinian Movement;③ event deposits caused by floods,earthquakes,etc.are developed in the Huangshanjie Formation;④ in the 4th Member,the dark mudstone is the rapid deposition of sufficient provenance under high accommodation;⑤ after the deposition of the Third Member of the Huangshanjie Formation,regional tectonic uplift and tectonic—sedimentary transformation occurred,and the provenance also became quasi-plain;⑥ there is a certain hiatus between the 4th Member and the underlying 3rd Member of Huangshanjie Formation and the overlying Taliqik Formation.Conclusions:The sedimentary characteristics of the Huangshanjie Formation in the Kuaq Depression are controlled by the tectonic evolution,forming three sedimentary cycles with different characteristics,and event sedimentary responses have occurred.There are hiatus both inside and at the top of the Huangshanjie Formation.

sedimentary characteristicssedimentary evolutionbraided-river deltameandering river deltaHuangshanjie FormationTriassicKuqa DepressionTarim Basin

王正和、程锦翔、张荣虎

展开 >

中国地质调查局成都地质调查中心(西南地质科技创新中心),成都,610218

自然资源部沉积盆地与油气资源重点实验室,成都,610218

中国石油杭州地质研究院,杭州,310023

中国石油勘探开发研究院塔里木盆地研究中心,新疆库尔勒,841000

展开 >

沉积特征 沉积演化 辫状河三角洲 曲流河三角洲 黄山街组 三叠系 库车坳陷 塔里木盆地

2025

地质论评
中国地质学会

地质论评

北大核心
影响因子:1.842
ISSN:0371-5736
年,卷(期):2025.71(1)