Comparison of modern fluid distribution, pressure and flow in sediments associated with anticlines growing in deepwater (Brunei) and continental environments (Iran)

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dc.contributor.authorMorley, C.
dc.contributor.authorWarren, J.
dc.contributor.authorTingay, M.
dc.contributor.authorBoonyasaknanon, P.
dc.contributor.authorJulapour, A.
dc.date.issued2014
dc.description.abstractAbstract not available
dc.description.statementofresponsibilityChris K. Morley, John Warren, Mark Tingay, Phathompat Boonyasaknanon, Ali Julapour
dc.identifier.citationMarine and Petroleum Geology, 2014; 51:210-229
dc.identifier.doi10.1016/j.marpetgeo.2013.11.011
dc.identifier.issn0264-8172
dc.identifier.issn1873-4073
dc.identifier.urihttp://hdl.handle.net/2440/114749
dc.language.isoen
dc.publisherElsevier
dc.rights© 2013 Elsevier Ltd. All rights reserved.
dc.source.urihttps://doi.org/10.1016/j.marpetgeo.2013.11.011
dc.subjectBrunei; Iran; overpressure; blow out; halite; smectite; fluid-escape
dc.titleComparison of modern fluid distribution, pressure and flow in sediments associated with anticlines growing in deepwater (Brunei) and continental environments (Iran)
dc.typeJournal article
pubs.publication-statusPublished

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