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    Dolomites in SE Asia.

    137400_20488_56233.pdf (350.0Kb)
    Access Status
    Open access
    Authors
    Carnell, A.
    Wilson, Moyra
    Date
    2003
    Type
    Conference Paper
    
    Metadata
    Show full item record
    Citation
    Carnell, Andrew and Wilson, Moyra. 2003. A review of dolomites in Southeast Asia, in 29th Annual Convention of the Indonesian Petroleum Association, pp. 207-217. Jakarta, Indonesia: Indonesian Petroleum Association.
    Source Title
    Proceedings of the Indonesian Petroleum Association, 29th Annual Convention
    Source Conference
    29th Annual Convention of the Indonesian Petroleum Association
    ISSN
    0126-1126
    Faculty
    Department of Applied Geology
    Faculty of Science and Engineering
    WA School of Mines
    Remarks

    This paper was originally published at the IPA Annual Convention, Jakarta 2003

    URI
    http://hdl.handle.net/20.500.11937/38579
    Collection
    • Curtin Research Publications
    Abstract

    This manuscript summarises published data on the distribution, habit, and current inferred models for dolomite occurrence in carbonates from southeast Asia. The presence of dolomite has significant implications for hydrocarbon exploration and production, as it may affect reservoir porosity, permeability, and connectivity to petroleum source areas. It may also be a factor in generation of undesirable non-hydrocarbon gases.This work is by no means exhaustive, given the paucity of published data on dolomites in the region, and there is considerable scope for further study. The extended abstract presented herein is modified from a review on SE Asian dolomites (Carnell and Wilson, submitted) submitted to a Geological Society of London Special Publication on ‘The Geometry & Petrogenesis of Dolomite Hydrocarbon Reservoirs’. The reader is referred to this Geological Society volume for the full manuscript, which contains descriptions of known SE Asian dolomites, discussions on their origins, together with maps, diagrams and tables showing the occurrence and characteristics of dolomites in Pre-Tertiary, Paleogene and Neogene carbonates.

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