Reservoir quality, textural evolution, and origin of fault-associated dolomites
| Main Authors: | , , , , , |
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| Format: | Journal Article |
| Published: |
American Association of Petroleum Geologists
2007
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| Online Access: | http://hdl.handle.net/20.500.11937/8563 |
| _version_ | 1848745694806933504 |
|---|---|
| author | Wilson, Moyra Evans, M Oxtoby, N Satria Nas, D Donnelly, T Thirlwall, Matthew |
| author_facet | Wilson, Moyra Evans, M Oxtoby, N Satria Nas, D Donnelly, T Thirlwall, Matthew |
| author_sort | Wilson, Moyra |
| building | Curtin Institutional Repository |
| collection | Online Access |
| first_indexed | 2025-11-14T06:21:26Z |
| format | Journal Article |
| id | curtin-20.500.11937-8563 |
| institution | Curtin University Malaysia |
| institution_category | Local University |
| last_indexed | 2025-11-14T06:21:26Z |
| publishDate | 2007 |
| publisher | American Association of Petroleum Geologists |
| recordtype | eprints |
| repository_type | Digital Repository |
| spelling | curtin-20.500.11937-85632018-12-14T00:47:30Z Reservoir quality, textural evolution, and origin of fault-associated dolomites Wilson, Moyra Evans, M Oxtoby, N Satria Nas, D Donnelly, T Thirlwall, Matthew 2007 Journal Article http://hdl.handle.net/20.500.11937/8563 10.1306/05070706052 American Association of Petroleum Geologists restricted |
| spellingShingle | Wilson, Moyra Evans, M Oxtoby, N Satria Nas, D Donnelly, T Thirlwall, Matthew Reservoir quality, textural evolution, and origin of fault-associated dolomites |
| title | Reservoir quality, textural evolution, and origin of fault-associated dolomites |
| title_full | Reservoir quality, textural evolution, and origin of fault-associated dolomites |
| title_fullStr | Reservoir quality, textural evolution, and origin of fault-associated dolomites |
| title_full_unstemmed | Reservoir quality, textural evolution, and origin of fault-associated dolomites |
| title_short | Reservoir quality, textural evolution, and origin of fault-associated dolomites |
| title_sort | reservoir quality, textural evolution, and origin of fault-associated dolomites |
| url | http://hdl.handle.net/20.500.11937/8563 |