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<http://digilib.unila.ac.id/id/eprint/58553> <http://purl.org/dc/terms/title> "PEMODELAN STRUKTUR BAWAH PERMUKAAN DAERAH PANAS\r\nBUMI BITTUANG, BERDASARKAN ANALISIS SECOND HORIZONTAL\r\nDERIVATIVE, SECOND VERTICAL DERIVATIVE, PEMODELAN 2.5D\r\n\r\nDAN 3D ANOMALI GAYA BERAT"^^<http://www.w3.org/2001/XMLSchema#string> .
<http://digilib.unila.ac.id/id/eprint/58553> <http://purl.org/ontology/bibo/abstract> "Daerah Bittuang, Tana Toraja, Sulawesi Selatan memiliki potensi panas bumi\r\nvulkanik. Panas Bumi Bittuang memiliki beberapa manifestasi yang muncul ke\r\npermukaan berupa air panas dan fumarol yang memiliki temperatur berkisar 39  ̊C\r\n– 96  ̊C. Pada sekitar area penelitian memiliki beberapa struktur geologi berupa\r\npatahan. Oleh karena itu, penelitian ini bertujuan untuk mencari struktur patahan\r\ndan mendapatkan nilai densitas daerah penelitian tersebut dengan menggunakan\r\ndata gaya berat. Pengolahan gaya berat pada penelitian ini dilakukan dengan\r\nmenentukan lebar jendela dengan analisis spektrum untuk digunakan pada filter\r\nmoving average agar mendapatkan zona anomali residual dan regional. Sedangkan\r\nuntuk menentukan struktur geologi dilakukan analisis Second Horizontal Deritive\r\ndan Second Vertical Derivative. Pada hasil pemodelan didapat nilai densitasnya\r\n2,35 gr/cc – 2.83 gr/cc pada model 2D kemudian 2,2 gr/cc – 3.0 gr/ cc pada model\r\n3D dengan batuan dasar berupa batuan malihan dan diketahui bahwa manifestasi\r\ndiduga memiliki hubungan dengan struktur patahan. Pada penelitian ini juga\r\nmenggunakan data tambahan berupa data peta kontur resistivitas semu untuk\r\nmenambah informasi mengenai daerah prospek\r\nThe Bittuang area, Tana Toraja, South Sulawesi has volcanic geothermal potential.\r\nBittuang Geothermal has several manifestations that appear to the surface in the\r\nform of hot water and fumaroles which have temperatures ranging from 39  ̊C - 96\r\n ̊C. In the vicinity of the study area has several geological structures in the form of\r\nfaults. Therefore, this study aims to find fault structures and obtain density values\r\nfor the study area using gravity data. Gravity processing in this research is done by\r\ndetermining the width of the window with spectrum analysis to be used in the\r\nmoving average filter in order to obtain residual and regional anomaly zones.\r\nMeanwhile, to determine the geological structure, a Second Horizontal Deritive and\r\nSecond Vertical Derivative analysis was performed. In the modeling results, the\r\ndensity value is 2.35 gr / cc - 2.83 gr / cc in the 2D model, then 2.2 gr / cc - 3.0 gr /\r\ncc in the 3D model with bedrock in the form of rocks and it is known that the\r\nmanifestations are thought to have a relationship with the structure fault. In this\r\nstudy also uses additional data in the form of apparent resistivity contour map data\r\nto add information about the geothermal prospect area."^^<http://www.w3.org/2001/XMLSchema#string> .
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