PETROGENESIS AND MINERALIZATION STUDY OF BAULA OPHIOLITE COMPLEX, KOLAKA, SOUTHEAST SULAWESI
Kolaka Regency is known as an area that produce nickel laterite deposit at East Sulawesi Ophiolite Belt (ESOB). One of ESOB trace is unveiled at study area, Baula District, Kolaka Regency. The study is worked by mapping and analyze ultramafic rock samples to determine ophiolite tectonic environment...
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id-itb.:240182017-10-03T11:29:43ZPETROGENESIS AND MINERALIZATION STUDY OF BAULA OPHIOLITE COMPLEX, KOLAKA, SOUTHEAST SULAWESI IRHAN MAIS CENDRAJAYA - NIM: 22014002, RIO Indonesia Theses INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/24018 Kolaka Regency is known as an area that produce nickel laterite deposit at East Sulawesi Ophiolite Belt (ESOB). One of ESOB trace is unveiled at study area, Baula District, Kolaka Regency. The study is worked by mapping and analyze ultramafic rock samples to determine ophiolite tectonic environment and identify its ore deposits beside nickel laterite. Petrographic and mineragraphic analysis as main analysis is worked to identify ultramafic rock minerals, ores, mineral paragenesis, and its tectonic environment. Magnetic susceptibiliy and serpentinite urat-urats analysis are also worked to support the main analysis. Based on all analysis, Baula Ophiolite Complex come under dismembered ophiolite formed in Mid Oceanic Ridge (MOR) tectonic environment. Chromite is identified as the abundant ore in the study area with NE–SW distribution, especially in harzburgit text |
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Kolaka Regency is known as an area that produce nickel laterite deposit at East Sulawesi Ophiolite Belt (ESOB). One of ESOB trace is unveiled at study area, Baula District, Kolaka Regency. The study is worked by mapping and analyze ultramafic rock samples to determine ophiolite tectonic environment and identify its ore deposits beside nickel laterite. Petrographic and mineragraphic analysis as main analysis is worked to identify ultramafic rock minerals, ores, mineral paragenesis, and its tectonic environment. Magnetic susceptibiliy and serpentinite urat-urats analysis are also worked to support the main analysis. Based on all analysis, Baula Ophiolite Complex come under dismembered ophiolite formed in Mid Oceanic Ridge (MOR) tectonic environment. Chromite is identified as the abundant ore in the study area with NE–SW distribution, especially in harzburgit |
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Theses |
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IRHAN MAIS CENDRAJAYA - NIM: 22014002, RIO |
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IRHAN MAIS CENDRAJAYA - NIM: 22014002, RIO PETROGENESIS AND MINERALIZATION STUDY OF BAULA OPHIOLITE COMPLEX, KOLAKA, SOUTHEAST SULAWESI |
author_facet |
IRHAN MAIS CENDRAJAYA - NIM: 22014002, RIO |
author_sort |
IRHAN MAIS CENDRAJAYA - NIM: 22014002, RIO |
title |
PETROGENESIS AND MINERALIZATION STUDY OF BAULA OPHIOLITE COMPLEX, KOLAKA, SOUTHEAST SULAWESI |
title_short |
PETROGENESIS AND MINERALIZATION STUDY OF BAULA OPHIOLITE COMPLEX, KOLAKA, SOUTHEAST SULAWESI |
title_full |
PETROGENESIS AND MINERALIZATION STUDY OF BAULA OPHIOLITE COMPLEX, KOLAKA, SOUTHEAST SULAWESI |
title_fullStr |
PETROGENESIS AND MINERALIZATION STUDY OF BAULA OPHIOLITE COMPLEX, KOLAKA, SOUTHEAST SULAWESI |
title_full_unstemmed |
PETROGENESIS AND MINERALIZATION STUDY OF BAULA OPHIOLITE COMPLEX, KOLAKA, SOUTHEAST SULAWESI |
title_sort |
petrogenesis and mineralization study of baula ophiolite complex, kolaka, southeast sulawesi |
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https://digilib.itb.ac.id/gdl/view/24018 |
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1821840744598470656 |