Peta Aliran Panas Dihubungkan Dengan Tatanan Tektonik Regional Di Daerah Selatan Busur Banda, Indonesia

This study located in Banda Arc relatively South West from Timor and North West from Australia. This location is very interesting to be studied with heat flow mapping because with this method can do hydrocarbon prospecting (also needed research with different methods), high heatflow value related wi...

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Main Authors: , Pandu Patria, , Salahuddin Husein, S.T., M.Sc., Ph.D.
Format: Theses and Dissertations NonPeerReviewed
Published: [Yogyakarta] : Universitas Gadjah Mada 2014
Subjects:
ETD
Online Access:https://repository.ugm.ac.id/130203/
http://etd.ugm.ac.id/index.php?mod=penelitian_detail&sub=PenelitianDetail&act=view&typ=html&buku_id=70618
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spelling id-ugm-repo.1302032016-03-04T08:07:20Z https://repository.ugm.ac.id/130203/ Peta Aliran Panas Dihubungkan Dengan Tatanan Tektonik Regional Di Daerah Selatan Busur Banda, Indonesia , Pandu Patria , Salahuddin Husein, S.T., M.Sc., Ph.D. ETD This study located in Banda Arc relatively South West from Timor and North West from Australia. This location is very interesting to be studied with heat flow mapping because with this method can do hydrocarbon prospecting (also needed research with different methods), high heatflow value related with hydrocarbon prospect. Tectonic setting for this area consist of trough, graben, platform, basin, and sub-basin with heatflow mapping that structural event can be differentiate. Heatflow is never measured directly but is obtained from the vertical component of the Fourier's Law, where the gradient in °C/km, thermal conductivity in W/mK and the heatflow Q in mW/m2. In this study the thermal conductivity calculation using three methods: Williams and Anderson, Houbolt and Wells and Demongodin (crossplot). 0,777 The results of the calculation of the thermal conductivity by several methods have a range of values for Williams and Anderson methods � 2,882 W m -1 K -1 , Houbolt and Wells 0,670 � 2,896 W m -1 K -1 and, Demongodin (crossplot) 1,920 � 2,410 W m -1 K -1 . Value range from calculation of heat flow is not too much for the method of Williams and Anderson 2,402 � 9,192 mW/m 2 , Houbolt and Wells 1,976 � 9,883 mW/m 2 and, Demongodin (crossplot) 4,774 � 10,536 mW/m 2 . The pattern of heatflow after the map was made following the regional tectonic in Timor area. Areas surrounding the basin have a high heat flow value, while the height of the area or platform has low heatflow values. Areas of research in the distribution of heatflow map has a high value is an area that has potential for oil and gas exploration. [Yogyakarta] : Universitas Gadjah Mada 2014 Thesis NonPeerReviewed , Pandu Patria and , Salahuddin Husein, S.T., M.Sc., Ph.D. (2014) Peta Aliran Panas Dihubungkan Dengan Tatanan Tektonik Regional Di Daerah Selatan Busur Banda, Indonesia. UNSPECIFIED thesis, UNSPECIFIED. http://etd.ugm.ac.id/index.php?mod=penelitian_detail&sub=PenelitianDetail&act=view&typ=html&buku_id=70618
institution Universitas Gadjah Mada
building UGM Library
country Indonesia
collection Repository Civitas UGM
topic ETD
spellingShingle ETD
, Pandu Patria
, Salahuddin Husein, S.T., M.Sc., Ph.D.
Peta Aliran Panas Dihubungkan Dengan Tatanan Tektonik Regional Di Daerah Selatan Busur Banda, Indonesia
description This study located in Banda Arc relatively South West from Timor and North West from Australia. This location is very interesting to be studied with heat flow mapping because with this method can do hydrocarbon prospecting (also needed research with different methods), high heatflow value related with hydrocarbon prospect. Tectonic setting for this area consist of trough, graben, platform, basin, and sub-basin with heatflow mapping that structural event can be differentiate. Heatflow is never measured directly but is obtained from the vertical component of the Fourier's Law, where the gradient in °C/km, thermal conductivity in W/mK and the heatflow Q in mW/m2. In this study the thermal conductivity calculation using three methods: Williams and Anderson, Houbolt and Wells and Demongodin (crossplot). 0,777 The results of the calculation of the thermal conductivity by several methods have a range of values for Williams and Anderson methods � 2,882 W m -1 K -1 , Houbolt and Wells 0,670 � 2,896 W m -1 K -1 and, Demongodin (crossplot) 1,920 � 2,410 W m -1 K -1 . Value range from calculation of heat flow is not too much for the method of Williams and Anderson 2,402 � 9,192 mW/m 2 , Houbolt and Wells 1,976 � 9,883 mW/m 2 and, Demongodin (crossplot) 4,774 � 10,536 mW/m 2 . The pattern of heatflow after the map was made following the regional tectonic in Timor area. Areas surrounding the basin have a high heat flow value, while the height of the area or platform has low heatflow values. Areas of research in the distribution of heatflow map has a high value is an area that has potential for oil and gas exploration.
format Theses and Dissertations
NonPeerReviewed
author , Pandu Patria
, Salahuddin Husein, S.T., M.Sc., Ph.D.
author_facet , Pandu Patria
, Salahuddin Husein, S.T., M.Sc., Ph.D.
author_sort , Pandu Patria
title Peta Aliran Panas Dihubungkan Dengan Tatanan Tektonik Regional Di Daerah Selatan Busur Banda, Indonesia
title_short Peta Aliran Panas Dihubungkan Dengan Tatanan Tektonik Regional Di Daerah Selatan Busur Banda, Indonesia
title_full Peta Aliran Panas Dihubungkan Dengan Tatanan Tektonik Regional Di Daerah Selatan Busur Banda, Indonesia
title_fullStr Peta Aliran Panas Dihubungkan Dengan Tatanan Tektonik Regional Di Daerah Selatan Busur Banda, Indonesia
title_full_unstemmed Peta Aliran Panas Dihubungkan Dengan Tatanan Tektonik Regional Di Daerah Selatan Busur Banda, Indonesia
title_sort peta aliran panas dihubungkan dengan tatanan tektonik regional di daerah selatan busur banda, indonesia
publisher [Yogyakarta] : Universitas Gadjah Mada
publishDate 2014
url https://repository.ugm.ac.id/130203/
http://etd.ugm.ac.id/index.php?mod=penelitian_detail&sub=PenelitianDetail&act=view&typ=html&buku_id=70618
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