A PRELIMINARY VIEW AND IMPORTANCE OF METAMORPHIC GEOLOGY FROM JIWO HILLS IN CENTRAL JAVA

Jiwo Hills is an isolated hill with approximately occupied 30 km 2 in Bayat area of Central Java. The Jiwo Hills has been considered to be composed of very low-grade metamorphic rocks. This contribution explains a preliminary view of the metamorphic rocks from collected rocks sample in the Ji...

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Main Authors: Nugroho Imam Setiawan, Nugroho, Yasuhito Osanai, Yasuhito, Carolus Prasetyadi, Carolus
Format: Article
Language:English
Published: Teknik Geologi Universitas Gadjah Mada 2013
Subjects:
Online Access:https://repository.ugm.ac.id/135116/1/11-23%20BPS02.pdf
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author Nugroho Imam Setiawan, Nugroho
Yasuhito Osanai, Yasuhito
Carolus Prasetyadi, Carolus
author_facet Nugroho Imam Setiawan, Nugroho
Yasuhito Osanai, Yasuhito
Carolus Prasetyadi, Carolus
author_sort Nugroho Imam Setiawan, Nugroho
collection UGM
description Jiwo Hills is an isolated hill with approximately occupied 30 km 2 in Bayat area of Central Java. The Jiwo Hills has been considered to be composed of very low-grade metamorphic rocks. This contribution explains a preliminary view of the metamorphic rocks from collected rocks sample in the Jiwo Hills. Common metamorphic rocks found in this area are phyllite, mica schist, calc-silicate schist, and marble with the foliation trend of NE-SW. Most of the metamorphic rock exposures are strongly weathered. Rarely epidote-glaucophane schist crop out near the exposure of serpentinite in western part of this complex. Several carbonate sedimentary rocks are converted to garnet-wollastonite skarn under the contact metamorphism probably caused by diabase intrusion. Garnet-wollastonite skarn mainly consists of garnet and wollastonite embed in the quartz matrix. The garnets are rich of grossular composition, range from Adr13–19Grs81–85Sps0–2. Those show anisotropic, with sectorial twinning zonings. The skarn deposits might give important information for economic resources in this area. Epidote-glaucophane schist mainly consists of glaucophane, epidote, quartz, phengite, titanite, and hematite. By the present of this blueschist facies of high-pressure metamorphic rock in this area, it confirms that Jiwo Hills is one of the high-pressure metamorphic terranes together with Luk Ulo Complex of Central Java, Meratus Complex of South Kalimantan, and Bantimala Complex of South Sulawesi. The serpentinites might facilitate exhumation of the blueschist in the Jiwo Hills. Detailed study of the distribution of metamorphic rocks in this area is needed in order to understanding tectonic evolution as well as economic geology. Keywords: Jiwo Hills, Bayat, blueschist, high-pressure metamorphic rocks, skarn
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spelling oai:generic.eprints.org:1351162015-09-04T01:53:14Z https://repository.ugm.ac.id/135116/ A PRELIMINARY VIEW AND IMPORTANCE OF METAMORPHIC GEOLOGY FROM JIWO HILLS IN CENTRAL JAVA Nugroho Imam Setiawan, Nugroho Yasuhito Osanai, Yasuhito Carolus Prasetyadi, Carolus Geology Jiwo Hills is an isolated hill with approximately occupied 30 km 2 in Bayat area of Central Java. The Jiwo Hills has been considered to be composed of very low-grade metamorphic rocks. This contribution explains a preliminary view of the metamorphic rocks from collected rocks sample in the Jiwo Hills. Common metamorphic rocks found in this area are phyllite, mica schist, calc-silicate schist, and marble with the foliation trend of NE-SW. Most of the metamorphic rock exposures are strongly weathered. Rarely epidote-glaucophane schist crop out near the exposure of serpentinite in western part of this complex. Several carbonate sedimentary rocks are converted to garnet-wollastonite skarn under the contact metamorphism probably caused by diabase intrusion. Garnet-wollastonite skarn mainly consists of garnet and wollastonite embed in the quartz matrix. The garnets are rich of grossular composition, range from Adr13–19Grs81–85Sps0–2. Those show anisotropic, with sectorial twinning zonings. The skarn deposits might give important information for economic resources in this area. Epidote-glaucophane schist mainly consists of glaucophane, epidote, quartz, phengite, titanite, and hematite. By the present of this blueschist facies of high-pressure metamorphic rock in this area, it confirms that Jiwo Hills is one of the high-pressure metamorphic terranes together with Luk Ulo Complex of Central Java, Meratus Complex of South Kalimantan, and Bantimala Complex of South Sulawesi. The serpentinites might facilitate exhumation of the blueschist in the Jiwo Hills. Detailed study of the distribution of metamorphic rocks in this area is needed in order to understanding tectonic evolution as well as economic geology. Keywords: Jiwo Hills, Bayat, blueschist, high-pressure metamorphic rocks, skarn Teknik Geologi Universitas Gadjah Mada 2013-12-11 Article PeerReviewed application/pdf en https://repository.ugm.ac.id/135116/1/11-23%20BPS02.pdf Nugroho Imam Setiawan, Nugroho and Yasuhito Osanai, Yasuhito and Carolus Prasetyadi, Carolus (2013) A PRELIMINARY VIEW AND IMPORTANCE OF METAMORPHIC GEOLOGY FROM JIWO HILLS IN CENTRAL JAVA. Prosiding Seminar Nasional Kebumian Ke-6 Teknik Geologi Universitas Gadjah Mada, 11-12 Desember 2013.
spellingShingle Geology
Nugroho Imam Setiawan, Nugroho
Yasuhito Osanai, Yasuhito
Carolus Prasetyadi, Carolus
A PRELIMINARY VIEW AND IMPORTANCE OF METAMORPHIC GEOLOGY FROM JIWO HILLS IN CENTRAL JAVA
title A PRELIMINARY VIEW AND IMPORTANCE OF METAMORPHIC GEOLOGY FROM JIWO HILLS IN CENTRAL JAVA
title_full A PRELIMINARY VIEW AND IMPORTANCE OF METAMORPHIC GEOLOGY FROM JIWO HILLS IN CENTRAL JAVA
title_fullStr A PRELIMINARY VIEW AND IMPORTANCE OF METAMORPHIC GEOLOGY FROM JIWO HILLS IN CENTRAL JAVA
title_full_unstemmed A PRELIMINARY VIEW AND IMPORTANCE OF METAMORPHIC GEOLOGY FROM JIWO HILLS IN CENTRAL JAVA
title_short A PRELIMINARY VIEW AND IMPORTANCE OF METAMORPHIC GEOLOGY FROM JIWO HILLS IN CENTRAL JAVA
title_sort preliminary view and importance of metamorphic geology from jiwo hills in central java
topic Geology
url https://repository.ugm.ac.id/135116/1/11-23%20BPS02.pdf
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