Growth history and facies evolution of the subis limestone - A carbonate platform exposed onshore Borneo Island, Malaysia

The Subis Limestone is a Member of the Tangap Formation. It is Upper Oligocene to Lower Miocene in age. The Subis Limestone is divided into two sequences which are different in depositional setting and architecture. The lower sequence is Upper Oligocene in age, generally deep marine depositional env...

Full description

Bibliographic Details
Main Authors: Dedeche, A., Pierson, B., Hunter, Aaron
Format: Conference Paper
Published: European Association of Geoscientists and Engineers, EAGE 2013
Online Access:http://hdl.handle.net/20.500.11937/15308
_version_ 1848748858175127552
author Dedeche, A.
Pierson, B.
Hunter, Aaron
author_facet Dedeche, A.
Pierson, B.
Hunter, Aaron
author_sort Dedeche, A.
building Curtin Institutional Repository
collection Online Access
description The Subis Limestone is a Member of the Tangap Formation. It is Upper Oligocene to Lower Miocene in age. The Subis Limestone is divided into two sequences which are different in depositional setting and architecture. The lower sequence is Upper Oligocene in age, generally deep marine depositional environment and is for the most part in the subsurface. The upper sequence is Lower Miocene in age, shallow marine reefal depositional environment and forms a spectacular limestone hill that reflects the original carbonate platform. The geomorphology, sedimentology and sequence stratigraphy of the platform (upper sequence) are studied in detail in this paper. The platform is found to be a good analogue to the Sarawak offshore carbonate platforms that mark one of the main hydrocarbon provinces in Southeast Asia for containing large reserves of natural gas and -to a lesser extent-oil.
first_indexed 2025-11-14T07:11:43Z
format Conference Paper
id curtin-20.500.11937-15308
institution Curtin University Malaysia
institution_category Local University
last_indexed 2025-11-14T07:11:43Z
publishDate 2013
publisher European Association of Geoscientists and Engineers, EAGE
recordtype eprints
repository_type Digital Repository
spelling curtin-20.500.11937-153082017-09-13T13:41:02Z Growth history and facies evolution of the subis limestone - A carbonate platform exposed onshore Borneo Island, Malaysia Dedeche, A. Pierson, B. Hunter, Aaron The Subis Limestone is a Member of the Tangap Formation. It is Upper Oligocene to Lower Miocene in age. The Subis Limestone is divided into two sequences which are different in depositional setting and architecture. The lower sequence is Upper Oligocene in age, generally deep marine depositional environment and is for the most part in the subsurface. The upper sequence is Lower Miocene in age, shallow marine reefal depositional environment and forms a spectacular limestone hill that reflects the original carbonate platform. The geomorphology, sedimentology and sequence stratigraphy of the platform (upper sequence) are studied in detail in this paper. The platform is found to be a good analogue to the Sarawak offshore carbonate platforms that mark one of the main hydrocarbon provinces in Southeast Asia for containing large reserves of natural gas and -to a lesser extent-oil. 2013 Conference Paper http://hdl.handle.net/20.500.11937/15308 10.3997/2214-4609.20130689 European Association of Geoscientists and Engineers, EAGE restricted
spellingShingle Dedeche, A.
Pierson, B.
Hunter, Aaron
Growth history and facies evolution of the subis limestone - A carbonate platform exposed onshore Borneo Island, Malaysia
title Growth history and facies evolution of the subis limestone - A carbonate platform exposed onshore Borneo Island, Malaysia
title_full Growth history and facies evolution of the subis limestone - A carbonate platform exposed onshore Borneo Island, Malaysia
title_fullStr Growth history and facies evolution of the subis limestone - A carbonate platform exposed onshore Borneo Island, Malaysia
title_full_unstemmed Growth history and facies evolution of the subis limestone - A carbonate platform exposed onshore Borneo Island, Malaysia
title_short Growth history and facies evolution of the subis limestone - A carbonate platform exposed onshore Borneo Island, Malaysia
title_sort growth history and facies evolution of the subis limestone - a carbonate platform exposed onshore borneo island, malaysia
url http://hdl.handle.net/20.500.11937/15308