ANALISIS STATUS EKSPLORASI UNTUK MENENTUKAN PROSPEKTIVITAS DI CEKUNGAN KUTAI

Kutai Basin exploration activity, East Kalimantan has been started since 19th century and continued until now. On the begining the exploration focus on the land of Kutai Basin, then with developing of exploration technology, the activity move forward to offshore then at 1995 to the deepwater. Right...

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Main Author: EKA SAPUTRA , SUNJAYA
Format: Theses
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/12688
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:12688
spelling id-itb.:126882017-09-27T14:38:36ZANALISIS STATUS EKSPLORASI UNTUK MENENTUKAN PROSPEKTIVITAS DI CEKUNGAN KUTAI EKA SAPUTRA , SUNJAYA Indonesia Theses INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/12688 Kutai Basin exploration activity, East Kalimantan has been started since 19th century and continued until now. On the begining the exploration focus on the land of Kutai Basin, then with developing of exploration technology, the activity move forward to offshore then at 1995 to the deepwater. Right now is been a basic question for doing exploration in Kutai Basin, How big the prospectivity still there? Which area are the most prospect? What play system which exist? And what exploration status are Kutai Basin? And how efficient the exploration activity in Kutai Basin. The Kutai Basin hierarchy is on the growth stage till early of mature stage, meanwhile the efficiency are 44.8% with discovery prediction are 18 to 22 million barrels oil equivalen. Creaming curve show that at least 4 pattern found, which can be interpreted showing the differencies of exploration play target in Kutai Basin. On pattern that show growth stage are pattern which show the play still have enough reserves to be found. Eocene Play, Oliogocene Carbonate Play and Miocene Carbonate Play on frontier stage, Early Miocene-Middle Deltaic Play and Miocene-Pliocene Turbiditic Deepwater Play on growth stage, meanwhile Middle Miocene-Pliocene Deltaic Play on mature stage to post mature stage, but had a rejuvination become early mature stage. Approach method of exploration hierarchy versus prospectivity can be used as referable base in determining the exploration strategy in basin or in exploration play. With pursuant to the data in this time, hence exploration to more beneficial to doing is exploration in Early Miocene-Middle Deltaic Play and Miocene-Pliocene Turbiditic Deepwater Play, while Eocene, Oligocene Carbonate and Miocene Carbonate Play although give enough prospectivity but still need the larger ones effort. In Middle Miocene-Pliocene Deltaic Play the exploration activity have to focus seeking of new trap or unconventional trap and also do the seeking by pass hydrocarbon zone. 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 Kutai Basin exploration activity, East Kalimantan has been started since 19th century and continued until now. On the begining the exploration focus on the land of Kutai Basin, then with developing of exploration technology, the activity move forward to offshore then at 1995 to the deepwater. Right now is been a basic question for doing exploration in Kutai Basin, How big the prospectivity still there? Which area are the most prospect? What play system which exist? And what exploration status are Kutai Basin? And how efficient the exploration activity in Kutai Basin. The Kutai Basin hierarchy is on the growth stage till early of mature stage, meanwhile the efficiency are 44.8% with discovery prediction are 18 to 22 million barrels oil equivalen. Creaming curve show that at least 4 pattern found, which can be interpreted showing the differencies of exploration play target in Kutai Basin. On pattern that show growth stage are pattern which show the play still have enough reserves to be found. Eocene Play, Oliogocene Carbonate Play and Miocene Carbonate Play on frontier stage, Early Miocene-Middle Deltaic Play and Miocene-Pliocene Turbiditic Deepwater Play on growth stage, meanwhile Middle Miocene-Pliocene Deltaic Play on mature stage to post mature stage, but had a rejuvination become early mature stage. Approach method of exploration hierarchy versus prospectivity can be used as referable base in determining the exploration strategy in basin or in exploration play. With pursuant to the data in this time, hence exploration to more beneficial to doing is exploration in Early Miocene-Middle Deltaic Play and Miocene-Pliocene Turbiditic Deepwater Play, while Eocene, Oligocene Carbonate and Miocene Carbonate Play although give enough prospectivity but still need the larger ones effort. In Middle Miocene-Pliocene Deltaic Play the exploration activity have to focus seeking of new trap or unconventional trap and also do the seeking by pass hydrocarbon zone.
format Theses
author EKA SAPUTRA , SUNJAYA
spellingShingle EKA SAPUTRA , SUNJAYA
ANALISIS STATUS EKSPLORASI UNTUK MENENTUKAN PROSPEKTIVITAS DI CEKUNGAN KUTAI
author_facet EKA SAPUTRA , SUNJAYA
author_sort EKA SAPUTRA , SUNJAYA
title ANALISIS STATUS EKSPLORASI UNTUK MENENTUKAN PROSPEKTIVITAS DI CEKUNGAN KUTAI
title_short ANALISIS STATUS EKSPLORASI UNTUK MENENTUKAN PROSPEKTIVITAS DI CEKUNGAN KUTAI
title_full ANALISIS STATUS EKSPLORASI UNTUK MENENTUKAN PROSPEKTIVITAS DI CEKUNGAN KUTAI
title_fullStr ANALISIS STATUS EKSPLORASI UNTUK MENENTUKAN PROSPEKTIVITAS DI CEKUNGAN KUTAI
title_full_unstemmed ANALISIS STATUS EKSPLORASI UNTUK MENENTUKAN PROSPEKTIVITAS DI CEKUNGAN KUTAI
title_sort analisis status eksplorasi untuk menentukan prospektivitas di cekungan kutai
url https://digilib.itb.ac.id/gdl/view/12688
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