Characteristics of the Triassic Source Rocks of the Aitutu Formation in the (West) Timor Basin

<p><span><a href="http://dx.doi.org/10.17014/ijog.v1i3.192">DOI:10.17014/ijog.v1i3.192</a></span></p><p>The Triassic rocks of the (West) Timor Basin have been identified that was mainly deposited in the  marine environment. The fine grained clastic...

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Main Authors: Asep Kurnia Permana, Aries Kusworo, Andi Heri Prastian
Format: Article
Language:English
Published: Geological Agency 2014-12-01
Series:Indonesian Journal on Geoscience
Subjects:
Online Access:https://ijog.geologi.esdm.go.id/index.php/IJOG/article/view/192
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author Asep Kurnia Permana
Aries Kusworo
Andi Heri Prastian
author_facet Asep Kurnia Permana
Aries Kusworo
Andi Heri Prastian
author_sort Asep Kurnia Permana
collection DOAJ
description <p><span><a href="http://dx.doi.org/10.17014/ijog.v1i3.192">DOI:10.17014/ijog.v1i3.192</a></span></p><p>The Triassic rocks of the (West) Timor Basin have been identified that was mainly deposited in the  marine environment. The fine grained clastics and carbonate  rocks of this Triassic marine  facies are considered to be the most promising source rocks potential in this basin. In this paper we present geochemical and petrographic data from outcrop samples of the Triassic carbonate Aitutu Formation, due to emphasized the organic maturation, kerogen type of the organic matter and the origin of the organic matter.  A representative of selected sample were subjected to the Rock-Eval Pyrolisis, vitrinite reflectance and thermal alteration index, bitumen extraction, were analyzed on the GC-MS. The samples were collected from marine deposit of the Triassic Sequence. The TOC values of the analyzed sample range between rich and rich organic richness (0.51% - 9.16%, wt.%, TOC), which consists mainly of type II and III kerogen and the organic matter consider to be predominantly oil/gas prone and gas prone potential. The thermal maturity assessed from T<sub>max</sub><sub>, </sub>TAI, and vitrinite reflectance shows an immature to early peak mature stage of the organic matter. The GC-MS analyses of the biomarkers indicate mainly the organic matter derived from mixed source rocks facies containing alga debris and higher plant terrestrial origin.</p>
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spelling doaj.art-abb54dee77534233bfe12b6ada5af5862022-12-21T23:10:08ZengGeological AgencyIndonesian Journal on Geoscience2355-93142355-93062014-12-011316517410.17014/ijog.1.3.165-174184Characteristics of the Triassic Source Rocks of the Aitutu Formation in the (West) Timor BasinAsep Kurnia Permana0Aries Kusworo1Andi Heri PrastianCenter for Geological SurveyCenter for Geological Survey<p><span><a href="http://dx.doi.org/10.17014/ijog.v1i3.192">DOI:10.17014/ijog.v1i3.192</a></span></p><p>The Triassic rocks of the (West) Timor Basin have been identified that was mainly deposited in the  marine environment. The fine grained clastics and carbonate  rocks of this Triassic marine  facies are considered to be the most promising source rocks potential in this basin. In this paper we present geochemical and petrographic data from outcrop samples of the Triassic carbonate Aitutu Formation, due to emphasized the organic maturation, kerogen type of the organic matter and the origin of the organic matter.  A representative of selected sample were subjected to the Rock-Eval Pyrolisis, vitrinite reflectance and thermal alteration index, bitumen extraction, were analyzed on the GC-MS. The samples were collected from marine deposit of the Triassic Sequence. The TOC values of the analyzed sample range between rich and rich organic richness (0.51% - 9.16%, wt.%, TOC), which consists mainly of type II and III kerogen and the organic matter consider to be predominantly oil/gas prone and gas prone potential. The thermal maturity assessed from T<sub>max</sub><sub>, </sub>TAI, and vitrinite reflectance shows an immature to early peak mature stage of the organic matter. The GC-MS analyses of the biomarkers indicate mainly the organic matter derived from mixed source rocks facies containing alga debris and higher plant terrestrial origin.</p>https://ijog.geologi.esdm.go.id/index.php/IJOG/article/view/192source rock potentialTriassic Aitutu Formation(West) Timor Basin
spellingShingle Asep Kurnia Permana
Aries Kusworo
Andi Heri Prastian
Characteristics of the Triassic Source Rocks of the Aitutu Formation in the (West) Timor Basin
Indonesian Journal on Geoscience
source rock potential
Triassic Aitutu Formation
(West) Timor Basin
title Characteristics of the Triassic Source Rocks of the Aitutu Formation in the (West) Timor Basin
title_full Characteristics of the Triassic Source Rocks of the Aitutu Formation in the (West) Timor Basin
title_fullStr Characteristics of the Triassic Source Rocks of the Aitutu Formation in the (West) Timor Basin
title_full_unstemmed Characteristics of the Triassic Source Rocks of the Aitutu Formation in the (West) Timor Basin
title_short Characteristics of the Triassic Source Rocks of the Aitutu Formation in the (West) Timor Basin
title_sort characteristics of the triassic source rocks of the aitutu formation in the west timor basin
topic source rock potential
Triassic Aitutu Formation
(West) Timor Basin
url https://ijog.geologi.esdm.go.id/index.php/IJOG/article/view/192
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AT arieskusworo characteristicsofthetriassicsourcerocksoftheaitutuformationinthewesttimorbasin
AT andiheriprastian characteristicsofthetriassicsourcerocksoftheaitutuformationinthewesttimorbasin