首页> 外文期刊>Geologia Croatica: a journal of the Institute of Geology Zagreb and Croatian Geological Society >Source Rock generative potential and volumetric characteristics of Kurrachine Dolomite Formation, Hayan Block, central Syrian Palmyrides
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Source Rock generative potential and volumetric characteristics of Kurrachine Dolomite Formation, Hayan Block, central Syrian Palmyrides

机译:叙利亚中部Palmyrides的Hayan区块Kurrachine白云岩组的烃源岩生矿潜力和体积特征

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Source rocks from the lower part of the Triassic Kurrachine Dolomite Formation were investigated in order to establish their role in the Petroleum System of the Hayan Block. Recent deep well discoveries accentuate the Triassic Kurrachine Dolomite Formation as a major play for hydrocarbon accumulations. The characteristic play definition is shown for the Hayan Block based on three defined elements: petroleum charge system, the source-reservoir formation characteristics and the trap-seal type. According to geochemical analyses, Triassic source rocks are of good generative potential, but they are not abundant (only thin layers were estimated). It was presumed that hydrocarbon generation and migration occurred from deeper Middle-Lower Palaeozoic Formations. Exploration results show that the generative potential of the Triassic source rocks in the Hayan Block was underestimated. Correlation and calibration of the petrophysical parameters from well logs and geochemical analyses show a much larger volume of mature source rocks than that predicted purely from geochemical analyses. The Kurrachine Dolomite Formation resistivity of 20 Ωm is typical of the area, and it represents the threshold value (Net Pay cutoff criteria) between immature and mature source rocks. Net Pay thickness (effective thickness), of mature and generative source rock intervals, exceeds more than 150 m in some wells. A calculated volumetric characteristic of source rocks indicates their high hydrocarbon generating capability. Intensive tectonic activity formed fractured zones as favourable reservoir rocks, so in some areas, practically no or very short migration pathways exist. Expelled hydrocarbons (within explored area) have not been accumulated into discrete reservoirs, thus the system is generating oil in situ. The results accentuate the existence of a key Triassic Petroleum System in the area of the Hayan Block. This Petroleum System incorporates the Triassic Kurrachine Dolomite, Amanus Shale Formations and the Permian Amanus Sand Formation.
机译:为了确定它们在哈安区块石油系统中的作用,对三叠纪Kurrachine白云岩层下部的烃源岩进行了研究。最近的深井发现使三叠纪的Kurrachine白云岩形成成为油气成藏的主要手段。基于三个定义的要素,显示了哈扬区块的特征层定义:石油装料系统,源-储层形成特征和圈闭类型。根据地球化学分析,三叠纪烃源岩具有良好的成矿潜力,但并不丰富(仅估计了薄层)。据推测,碳氢化合物的产生和运移发生在较深的中下古生界地层。勘探结果表明,三叠纪烃源岩的生矿潜力被低估了。来自测井和地球化学分析的岩石物理参数的相关和校准显示,与纯粹根据地球化学分析预测的相比,成熟烃源岩的体积要大得多。典型的区域是20Ωm的Kurrachine白云岩地层电阻率,它代表了未成熟和成熟烃源岩之间的阈值(净产值截止标准)。在某些井中,成熟和生烃源岩层段的净净厚度(有效厚度)超过150 m。计算出的烃源岩体积特征表明它们具有很高的生烃能力。强烈的构造活动将裂缝带形成为有利的储集岩,因此在某些地区,几乎没有或仅有很短的运移路径。驱出的碳氢化合物(在勘探范围内)尚未积累到离散的油藏中,因此该系统在现场采油。结果强调了哈扬区块地区主要的三叠纪石油系统的存在。该石油系统包含了三叠纪的Kurrachine白云岩,Amanus页岩地层和二叠纪Amanus砂岩地层。

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