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Complex Stratigraphic and Structural Evolution of Jabung Subbasin and ItsHydrocarbon Accumulation: Case Study From Lower Talang Akar Reservoir,South Sumatra Basin, Indonesia

机译:贾邦次盆地的复杂地层和构造演化及其油气成藏:以印度尼西亚南苏门答腊盆地塔朗阿卡下部储层为例

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Combined stratigraphic and structural traps of LowerrnTalang Akar Formation (LTAF) syn-rift deposits create arntypical play type in South Sumatra Basin, Indonesia.rnThree field examples from Jabung Block show pop-uprnfeatures caused by Plio-Pleistocene tectonics invertingrnthe pre-existing structures. This phenomenon createsrnthe major hydrocarbon traps in the Jabung (Tungkal)rnsub-basin providing strong targets for further explorationrnwork.rnIncorporating existing 3D seismic and wireline log data,rna tectono-sedimentary model unique for the each fieldrnwas generated. All three field geological models are inrnclose proximity to each other within the Betara Complex.rnGenerally, there are three distinct identifiable sub-basinrnevolution periods. First, a period of horst-grabenrndevelopment controlled by major localized extensionalrnfaults that initiated the basin architecture. This episodernwas followed by rapid to moderate sedimentationrncontrolled by normal faults resulting in deposition ofrnOligocene Talang Akar alluvial, fluvial and deltaicrndeposits. Secondly, a period of decreased fault activityrnalong with regional subsidence coinciding with therndeposition of post-rifting fine marine Miocene sedimentsrnwhich provided a regional seal for the underlyingrnreservoirs. The third period is marked by regional upliftrnresulting in wide spread basin inversion over the entirernregion providing a period of hydrocarbon trapping.rnBasin evolution provided complex stratigraphic andrnstructural features and constitutes compartmentalized reservoirs. Complex-multiple gas and oil contacts andrnvariation in CO2 distribution has verified the complexityrnof the basins geological framework.rnDrainage patterns identified from localized paleogeographicrnconfigurations can be used to locaternsedimentary styles and trends. When combined withrnattribute extractions and structural analysis, thesernpatterns can help explorationists develop excellentrnopportunities for further exploration and development ofrnthe area.
机译:下印尼塔朗阿卡组(LTAF)同裂陷沉积物的组合地层和构造圈闭在印度尼西亚南苏门答腊盆地形成了典型的游动类型。三个Jabung区块的田间实例显示了由上新世构造运动使原有结构反转而引起的弹出特征。这种现象在Jabung(Tungkal)子盆地中形成了主要的油气藏,为进一步的勘探提供了强有力的目标。rnr结合了现有的3D地震和电缆测井数据,生成了每个油田特有的构造-沉积模型。在Betara复杂区内,所有这三个野外地质模型都彼此紧邻。通常,存在三个不同的可识别的亚盆地演化时期。首先,一段由主要的局部伸展断裂控制的地貌发展期开始了盆地构造。此后是由正常断层控制的快速到中度沉积,导致渐新世塔朗阿卡河冲积,河流和三角洲沉积物的沉积。其次,断层活动减少的时期伴随着区域沉降,这与裂谷后精细的海洋中新世沉积物的沉积相吻合,这为下伏的储层提供了区域封闭。第三阶段的特征是区域隆升,导致整个区域内大范围的盆地反转,从而提供了一个油气成藏期。盆地的演化提供了复杂的地层和结构特征,并构成了分隔储层。复杂多样的油气接触以及CO2分布的变化已经证实了盆地地质框架的复杂性。从局部古地理构造确定的排水模式可用于确定沉积样式和趋势。与属性提取和结构分析结合使用时,这些模式可以帮助勘探人员开发出极好的机会,以进一步勘探和开发该地区。

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