Delineasi Zona Prospek Sistem Panasbumi Daerah ‘P’ Menggunakan Pemodelan Multi Dimensi Data Magnetotelurik Terintegrasi Data Geologi dan Geokimia

Puji Suharmanto, Yunus Daud, ahmad zarkasyi
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Abstract

A study for delineating geothermal system of prospect area “P” has been done by using multi-dimensional modeling of magnetotelluric data. Physiographycally, geothermal prospect of “P” area is located at non-volcanic Banda inner arc hosted by Malihan Sekis rock complex with Perm-Trias age. The existance of geothermal system in this area is indicated by the presence of thermal manifestations in form of 6 chloride-bicarbonate hot springs with temperature in the the range of 37-67oC, and pH of 6-7. The development of geothermal system is most probably associated with strong tectonic activity caused by the collision between Seram island plate and Australian plate that ignite the occurence of intrussive body as heat source. In order to know the subsurface information of prospect area, magnetotelluric (MT) survey has been done. The processing of MT data was started from time-series data, continued by noise filtering, rotation of strike orientation and static shift correction to obtain better MT curve. The data were then being inversed by means of 1-Dimensional, 2-Dimensional and 3-Dimensional inversion methods. Reservoir temperature is estimated to be around 160-180 oC and classified as moderate temperature. The result of MT data inversions shows the presence of conductive layer ( 300 ?m) with updome shape appears underneath the manifestations occurence (MAP1, MAP2, MAP4, and MAP5), indicating that the heat source is located in northern part and elongate to souteast direction. The conceptual model of geothermal system was built based on integrated interpretation of geological, geochemical and geophysical data. The prospect area and recommendation of drilling location is estimated to be ± 3 km2 around upflow zone. Keywords: Prospect zone, geothermal system, magnetotelluric method, multi-dimension modeling
P系统热前景区核聚变利用地质学和地球化学数据的多维集成模型
利用大地电磁数据的多维建模方法,对勘探区“P”的地热系统进行了刻画研究。从物理地理上看,“P”地区的地热勘探区位于Malihan Sekis岩石杂岩的非火山班达内弧,具有Perm Trias年龄。该地区地热系统的存在表现为6个氯化物-碳酸氢盐温泉的热表现,温度在37-67oC之间,pH为6-7。地热系统的发展很可能与瑟兰岛板块与澳大利亚板块碰撞引起的强烈构造活动有关,该活动点燃了作为热源的侵入体的出现。为了了解勘探区的地下信息,进行了大地电磁测量。MT数据的处理从时间序列数据开始,继续进行噪声滤波、走向旋转和静态偏移校正,以获得更好的MT曲线。然后通过一维、二维和三维反演方法对数据进行反演。储层温度估计在160-180℃左右,属于中等温度。MT数据反演结果表明,在表现物(MAP1、MAP2、MAP4和MAP5)的下方出现了呈上升体形状的导电层(300?m),表明热源位于北部并向东南方向延伸。基于地质、地球化学和地球物理数据的综合解释,建立了地热系统的概念模型。预计上行带周围的勘探区域和钻井位置建议为±3km2。关键词:勘探区、地热系统、大地电磁法、多维建模
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