布格异常解释确定婆罗湾-依真热区断层和地下结构

Anjar Pranggawan Azhari, S. Maryanto, A. Rachmansyah
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引用次数: 5

摘要

利用Lacoste & Romberg G-1035重力仪在Blawan-Ijen地热区进行了重力测量。这是之前研究的重点研究。通过重力数据约简、水平面约简、向上延拓得到残差布格异常数据。布格异常解释结果显示新断层的出现及其相对运动。Blawan故障(F1)、F2、F3、F6为正常故障。布拉万断裂是控制布拉万-伊真地热区的主要断裂。F4和F5为斜向断裂,在班尤帕希特河形成地堑。F7为反向故障。地下模式显示,勃拉万—伊真热区以伊真火山口为主,形成火成岩(ρ1=2.670 g/cm3)、嵌套页岩和砂岩(ρ2=2.644 g/cm3)为勃拉万湖沉积,岩浆侵入岩(ρ3=2.814 g/cm3和ρ7=2.821 g/cm3)、安山岩(ρ4=2.448 g/cm3)为地热储层,Blau山火山碎屑气降沉积(ρ5=2.613 g/cm3)和熔岩流(ρ6=2.890 g/cm3)。
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INTERPRETATION OF BOUGUER ANOMALY TO DETERMINE FAULT AND SUBSURFACE STRUCTURE AT BLAWAN-IJEN GEOTHERMAL AREA
Gravity survey has been acquired by Gravimeter Lacoste & Romberg G-1035 at Blawan-Ijen geothermal area. It was a focusing study from previous research. The residual Bouguer anomaly data was obtain after applying gravity data reduction, reduction to horizontal plane, and upward continuation. Result of Bouguer anomaly interpretation shows occurrence of new faults and their relative movement. Blawan fault (F1), F2, F3, and F6 are normal fault. Blawan fault is main fault controlling hot springs at Blawan-Ijen geothermal area. F4 and F5 are oblique fault and forming a graben at Banyupahit River. F7 is reverse fault. Subsurface model shows that Blawan-Ijen geothermal area was dominated by the Ijen caldera forming ignimbrite (ρ1=2.670 g/cm3), embedded shale and sand (ρ2=2.644 g/cm3) as Blawan lake sediments, magma intrusion (ρ3=2.814 g/cm3 & ρ7=2.821 g/cm3), andesite rock (ρ4=2.448 g/cm3) as geothermal reservoir, pyroclastic air fall deposits (ρ5=2.613 g/cm3) from Mt. Blau, and lava flow (ρ6=2.890 g/cm3).
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