Characteristics of repeated, detached, Miocene–Pliocene tectonic inversion events, in a large delta province on an active margin, Brunei Darussalam, Borneo
Authors:
- C.K. MorleyCMC.K. Morley
- S. BackSBS. Back
- P. Van RensbergenPRP. Van Rensbergen
- P. CrevelloPCP. Crevello
- J.J. LambiaseJLJ.J. Lambiase
- 1 July 2003
- journal article
- Published by Elsevier in Journal of Structural Geology
- Vol. 25 (7) , 1147-1169
Abstract
No abstract availableKeywords
This publication has 16 references indexed in Scilit:
- Depositional Environment and Sequence Stratigraphy of Miocene Deltaic Cycles Exposed along the Jerudong Anticline, Brunei DarussalamJournal of Sedimentary Research, 2001
- A Miocene collisional belt in north Borneo: uplift mechanism and isostatic adjustment quantified by thermochronologyJournal of the Geological Society, 2000
- Shale tectonics and deformation associated with active diapirism: the Jerudong Anticline, Brunei DarussalamJournal of the Geological Society, 1998
- Comparison of gravity‐driven deformation styles and behavior associated with mobile shales and saltTectonics, 1996
- Reconstructing Cenozoic SE AsiaGeological Society, London, Special Publications, 1996
- The ‘Rajang accretionary prism’ and ‘Lupar Line’ problem of BorneoGeological Society, London, Special Publications, 1996
- Estimating inversion: results from clay modelsGeological Society, London, Special Publications, 1995
- Tertiary tectonic evolution of the NW Sabah Continental MarginBulletin of the Geological Society of Malaysia, 1993
- The nature and significance of regional unconformities in the hydrocarbon-bearing Neogene sequence offshore West SabahBulletin of the Geological Society of Malaysia, 1987
- Structural Styles in Western Sabah OffshoreBulletin of the Geological Society of Malaysia, 1980