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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Main Author: IRHAN MAIS CENDRAJAYA - NIM: 22014002, RIO
Format: Theses
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/24018
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:24018
spelling 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
institution Institut Teknologi Bandung
building Institut Teknologi Bandung Library
continent Asia
country Indonesia
Indonesia
content_provider Institut Teknologi Bandung
collection Digital ITB
language Indonesia
description 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
format Theses
author IRHAN MAIS CENDRAJAYA - NIM: 22014002, RIO
spellingShingle 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
url https://digilib.itb.ac.id/gdl/view/24018
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