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OALib Journal期刊
ISSN: 2333-9721
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准噶尔盆地东部滴水泉地区侏罗系八道湾组沉积特征与沉积演化模式
Keywords: 准噶尔盆地,滴水泉地区,八道湾组,沉积特征,演化模式
Abstract:
？在对区域地质、岩心、测井及地震资料分析的基础上，研究了准噶尔盆地东部滴水泉地区侏罗系八道湾组沉积特征、沉积相展布特征及沉积演化模式。结果表明:研究区八道湾组主要发育辫状河、辫状河三角洲和湖泊3种沉积相类型，可进一步细分为辫状河道、泛滥平原、辫状河三角洲平原、辫状河三角洲前缘及滨浅湖5种亚相类型，以及水道、心滩、湿地、分流河道、水下分流河道、支流间湾、河口坝、远砂坝和滨浅湖泥9种微相类型。j1b1段沉积期，由北东方向的克拉美丽山提供物源，分别向南、向西发育大范围砾质辫状河沉积；j1b2段沉积期，湖进开始由南西向北东方向上超，湖泊范围可达研究区内的古剥蚀区，分布了广阔的湖泊相沉积；j1b3段沉积期，构造活动强烈，物源供给充沛，大量碎屑物从克拉美丽山进入滴水泉地区，形成辫状河三角洲沉积。准噶尔盆地侏罗纪沉积环境及背景条件具有“沟梁相间、盆大水浅、河长扇短、源多坡缓”的特点，结合研究区的沉积特征及沉积展布特征，提出研究区为辫状河—湖泊—辫状河三角洲相结合的沉积演化模式。
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