首页> 外文期刊>Acta Geologica Sinica - English Edition >Provenance System Analysis of the Nantun Formation of the Huhehu Sag in Hailar Basin
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Provenance System Analysis of the Nantun Formation of the Huhehu Sag in Hailar Basin

机译:海拉尔盆地呼和湖凹陷南屯组物源系统分析

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Huhehu Sag is a new battlefield for the future oil and gas exploration in the Hailar Basin. At present, exploration of this area stays at a low level and the understanding of the provenance system of the Nantun Formation is comparatively weak. So, to carry out the detailed depiction of the provenance system in the study area is significant for the sedimentary system reconstruction, for the prediction of reservoir distribution and favorable areas. Based on comprehensive analysis of paleogeomorphy, light-heavy mineral and seismic reflection features, sandstone thickness and sandstone percentage, this paper analyzes in detail the provenance system of the Nantun Formation in Huhehu Sag from various angles and levels. It shows that provenances of the Huhehu Sag mainly originated from the eastern Xilinbeier Salient and western Bayan Mountain Uplift. The provenances surrounding the lake basin converged to the center of the basin, among which, the steep slope belt and the gentle slope belt are the main provenances, and the southern uplift is a secondary one. The distribution framework of the provenance fundamentally determines the distribution rules of the depositional system and its sand body developing during the Nantun period.
机译:呼和浩凹陷是海拉尔盆地未来油气勘探的新战场。目前,该地区的勘探工作仍处于较低水平,对南屯组物源体系的了解相对薄弱。因此,在研究区进行物源系统的详细描述,对沉积系统的重建,储层分布和有利区的预测具有重要意义。在综合分析古地貌,轻矿物和地震反射特征,砂岩厚度和砂岩百分比的基础上,从不同角度和层次详细分析了呼和湖凹陷南屯组物源系统。结果表明,呼和湖凹陷的物源主要来自锡林贝尔东部凸起和白云山凸起西部。湖盆周围种源汇聚到盆地中心,其中陡坡带和缓坡带是主要种源,南部隆起是次要种源。物源的分布框架从根本上决定了南屯时期沉积体系及其砂体发育的分布规律。

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