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Geomorphology of research area is divided into four units, they are Fault Block Mountain, Anticlinal Valley, Homoclinal Ridge and Alluvial Plain Units. A geological research shows that there are six litologic units exposed, from the oldest to the youngest, Claystone, Volcanic Breccia, Limestone, San...
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id-itb.:135702017-09-27T11:46:45Z#TITLE_ALTERNATIVE# HAMZAH (NIM 12006043), IRFA Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/13570 Geomorphology of research area is divided into four units, they are Fault Block Mountain, Anticlinal Valley, Homoclinal Ridge and Alluvial Plain Units. A geological research shows that there are six litologic units exposed, from the oldest to the youngest, Claystone, Volcanic Breccia, Limestone, Sandstone, Pyroclastic Breccia and Alluvial Units. Structure developed in the area, consists of reverse fault and anticline with W – E direction and strike-slip fault with NW – SE direction. The reverse fault which located in the southern part of the research area seems to control the presence of hotspring near the Cimandiri River. Based on the stable isotope analysis of δD and δ18O in the research area indicates that hot springs are meteoric origin and part of outflow of the Salak geothermal system. text |
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Geomorphology of research area is divided into four units, they are Fault Block Mountain, Anticlinal Valley, Homoclinal Ridge and Alluvial Plain Units. A geological research shows that there are six litologic units exposed, from the oldest to the youngest, Claystone, Volcanic Breccia, Limestone, Sandstone, Pyroclastic Breccia and Alluvial Units. Structure developed in the area, consists of reverse fault and anticline with W – E direction and strike-slip fault with NW – SE direction. The reverse fault which located in the southern part of the research area seems to control the presence of hotspring near the Cimandiri River. Based on the stable isotope analysis of δD and δ18O in the research area indicates that hot springs are meteoric origin and part of outflow of the Salak geothermal system. |
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Final Project |
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HAMZAH (NIM 12006043), IRFA |
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HAMZAH (NIM 12006043), IRFA #TITLE_ALTERNATIVE# |
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HAMZAH (NIM 12006043), IRFA |
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HAMZAH (NIM 12006043), IRFA |
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https://digilib.itb.ac.id/gdl/view/13570 |
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1820736225466646528 |