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Geochemical Characteristics and Logging Quantitative Prediction Model Establishment of Source Rocks in Saline Lake Basin-Take the Paleogene of Qaidam Basin as an Example

机译:盐湖池源岩石源岩石地球化学特征及测井定量预测模型为例

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The western Qaidam basin in China is an inland salt lake basin in the Cenozoic arid climate.In recent years,significant breakthroughs have been made in oil and gas exploration in the paleogene lower Ganchaigou formation(E3)in this area,and 200 million tons reserves have been discovered.It is proved that the paleogene saline lacustrine source rocks have great potential.Salt lake source rocks in the study area are obviously different from freshwater lake sediments,and their main characteristics are the mixed deposits of hydrocarbon source rocks and salt rocks,gypsum,carbonate rocks and terrigenous clastic rocks,with strong heterogeneity,and the thickness of single layer of source rocks is thin,generally 1.5-3.0 m.The TOC value of source rocks ranges from 0.27% to 1.11%,and the effective source rocks(TOC>0.4%)account for 56.25%.Chloroform asphalt"A"of source rocks ranges from 0.03% to 0.58%,and the effective source rock(chloroform asphalt"A">0.015%)accounts for 100%.In order to quantitatively identify and evaluate the hydrocarbon source rocks in the region.A quantitative model is established between the comprehensive lithological characteristics of logging information and the organic carbon mass fraction,and the hydrocarbon source rock is predicted longitudinally.In contrast optimization on the basis of logging information,the establishment of natural gamma ray-resistivity curve overlapping method(qualitative)quantitative prediction model,according to the comparison of the measured values and the fitted value,when GR logging curve>95 API,RD>40 Ω m.mudstone and grey mudstone as the effective hydrocarbon source rocks in the area,the quantitative prediction model fitting effect is good,the oil and gas resources for the area provides a method for quick support.
机译:中国西部柴达木盆地是一家内省新生代干旱气候的内陆盐湖盆地。近年来,在该地区的古代古古沟地板(E3)古古代下的石油和天然气勘探中取得了重大突破,储备了200万吨已被发现。古代盐水曲线源岩有很大的潜力。研究区域的湖泊源岩显然与淡水湖泊沉积物不同,其主要特点是碳氢化合物源岩和盐岩的混合沉积物,石膏,碳酸盐岩石和鸡肉碎屑岩,具有强的异质性,单层源岩的厚度薄,一般为1.5-3.0 m。源岩的TOC值范围为0.27%至1.11%,而有效的源岩(TOC> 0.4%)占56.25%。氯仿沥青“A”的源极岩的范围从0.03%到0.58%,有效的源岩(氯仿沥青“A”> 0.015%)占100%。 Quantitati.在识别和评估该区域中的烃源岩。在测井信息的综合岩性特征和有机碳质量分数之间建立了定量模型,并且甘油源岩被纵向预测。在伐木信息的基础上对比度优化,建立天然伽马射线电阻率曲线重叠方法(定性)定量预测模型,根据测量值和装配值的比较,当GR测井曲线> 95 API,RD>40Ωm.mudstone和灰泥岩作为该地区有效的烃源岩,定量预测模型拟合效果良好,该区域的石油和天然气资源提供了一种快速支持的方法。

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