北苏门答腊曼德勒纳塔尔省索里克马拉皮地热储层的确定

M. S. Hidayatullah, A. Haryanto, J. Hutabarat, R. Hidayat
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引用次数: 0

摘要

Sorik Marapi地热发电厂(SMGP)位于北苏门答腊的Mandailing Natal(距棉兰东南350公里)。该研究需要从地表表现对蚀变矿物资料进行验证,并结合流体地球化学特征,确定生产井的地热储层带。因此,使用了地温计和地理指示器计算。对探井的38个地表形态和11个切削样进行了室内试验。这一地区的表现包括温泉、喷气孔和热气腾腾的地面。研究区发现的蚀变矿物有硬石膏、绿帘石、方解石、绿泥石、白云母、叶蜡石、沸石等。蚀变带主要分布在沸石带、绿帘石带和硬石膏绢云母带。地表和生产井含氯化物水、硫酸盐水、硫酸盐-氯化物水和碳酸氢盐水的地球化学特征。SH-01井储层温度范围为240 ~ 280℃,SH-02井储层温度范围为249.89 ~ 302.92℃,SH-03井储层温度范围为231.09 ~ 280℃。将矿物地温计计算与地球化学流体地温计进行了对比,得到了有效的结果。从两个地温计估计的储层温度可以看出这一点。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
etermination of Geothermal Reservoir Zone of Sorik Marapi, Mandailing Natal, North Sumatra
The Sorik Marapi Geothermal Power (SMGP) Field is located in Mandailing Natal (350 km to the southeast from Medan), North Sumatra. This study needed alteration mineral data validation with fluid geochemical characteristics from surface manifestations, and production wells were determined the geothermal reservoir zone. Therefore geothermometer and geoindicator calculations were used. Laboratory tests were carried out on 38 surface manifestations and 11 cutting samples of exploration well. Manifestations in this area include hot springs, fumaroles, and steaming ground. Alteration minerals found in the study area are anhydrite, epidote, calcite,chlorite, muscovite, pyrophyllite, and zeolite. The alteration zone is located in the zeolite zone, the epidote zone,and the anhydrite-sericite zone. Geochemical manifestations of surface and production wells containing chloride water, sulfate water, sulfate-chloride water, and bicarbonate water. The estimated reservoir temperature of SH-01 well shows temperatures ranging from 240–280˚C, SH-02 well shows temperatures of 249.89–302.92˚C, SH-03 well show temperatures of 231.09–280˚C. The mineral geothermometer calculation, which is correlated with the geochemical fluid geothermometer, shows valid results. This is evident from the estimated reservoir temperatures of the two geothermometers.
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