准噶尔盆地南缘多断裂控制冲断构造与深部油气勘探目标

IF 8 Q1 ENERGY & FUELS
Baoli YU , Chengzao JIA , Keyu LIU , Yong DENG , Wei WANG , Peng CHEN , Chao LI , Jia CHEN , Boyang GUO
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引用次数: 0

摘要

准噶尔盆地南缘前陆冲断带深部勘探前景不明朗,控制构造变形、古构造和滑脱层分布、主要烃源岩分布等因素均存在不确定性。基于最新的三维地震、重磁、钻井资料,结合前期构造物理模拟和离散元数值模拟实验结果,系统表征了准噶尔盆地南部深层既有古构造和滑脱层的空间分布,分析了构造变形特征和形成机制。明确了多套烃源岩的分布规律,重新评价了重点带的油气成藏特征。展望了具有突破可能性的深部下组合的勘探目标。得到了三个方面的关键结果。首先,构造变形受两期古构造和3个横向变化明显的滑脱层控制,即侏罗系(厚度适中、分布广泛)、白垩纪(滑脱层最厚但较弱)和古近系(滑脱层较薄但长距离侧向冲断)。据此,确定了四层复合变形层序,构造成因模式为横向分段控制古隆起带、纵向多剥离层序控制构造带。②首次将高精度重磁资料与时频电磁资料相结合,刻画出二叠系烃源岩西呈窄槽、中呈多凹陷、东呈宽盆地的分布格局,侏罗系烃源岩西泥岩较厚,东煤富集。第三,根据构造变形强度、圈闭有效性和源-圈闭配置,建立了2个含油气系统和4层复合成藏模式。将准噶尔盆地南部划分为3段10个带,提出了该地区深部组合的分级勘探策略,即重点关注5个优先带,向3个潜在区扩展,挑战2个高风险靶区。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Multi-detachment-controlled thrust structures and deep hydrocarbon exploration targets in southern margin of Junggar Basin, NW China
For deep prospects in the foreland thrust belt, southern Junggar Basin, NW China, there are uncertainties in factors controlling the structural deformation, distribution of paleo-structures and detachment layers, and distribution of major hydrocarbon source rocks. Based on the latest 3D seismic, gravity-magnetic, and drilling data, together with the results of previous structural physical simulation and discrete element numerical simulation experiments, the spatial distribution of pre-existing paleo-structures and detachment layers in deep strata of southern Junggar Basin were systematically characterized, the structural deformation characteristics and formation mechanisms were analyzed, the distribution patterns of multiple hydrocarbon source rock suites were clarified, and hydrocarbon accumulation features in key zones were reassessed. The exploration targets in deep lower assemblages with possibility of breakthrough were expected. Key results are obtained in three aspects. First, structural deformation is controlled by two-stage paleo-structures and three detachment layers with distinct lateral variations: the Jurassic layer (moderate thickness, wide distribution), the Cretaceous layer (thickest but weak detachment), and the Paleogene layer (thin but long-distance lateral thrusting). Accordingly, a four-layer composite deformation sequence was identified, and the structural genetic model with paleo-bulge controlling zonation by segments laterally and multiple detachment layers controlling sequence vertically. Second, the Permian source rocks show a distribution pattern with narrow trough (west), multiple sags (central), and broad basin (east), which is depicted by combining high-precision gravity-magnetic data and time-frequency electromagnetic data for the first time, and the Jurassic source rocks feature thicker mudstones in the west and rich coals in the east according to the reassessment. Third, two petroleum systems and a four-layer composite hydrocarbon accumulation model are established depending on the structural deformation strength, trap effectiveness and source-trap configuration. The southern Junggar Basin is divided into three segments with ten zones, and a hierarchical exploration strategy is proposed for deep lower assemblages in this region, that is, focusing on five priority zones, expanding to three potential areas, and challenging two high-risk targets.
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