Architectural and facies organization of slope channel fills : Upper Cretaceous Rosario Formation, Baja California, Mexico
| dc.contributor.author | Li, Pan | |
| dc.contributor.author | Kneller, Benjamin Charles | |
| dc.contributor.author | Thompson, Philip | |
| dc.contributor.author | Bozetti, Guilherme | |
| dc.contributor.author | Dos Santos, Thisiane | |
| dc.contributor.institution | University of Aberdeen.Geology and Geophysics | en |
| dc.contributor.institution | University of Aberdeen.Geosciences | en |
| dc.date.accessioned | 2018-11-28T00:02:52Z | |
| dc.date.available | 2018-11-28T00:02:52Z | |
| dc.date.embargoedUntil | 2018-11-28 | |
| dc.date.issued | 2018-04-01 | |
| dc.description | This work comprised part of PL’s PhD study, which was funded by the China Scholarship Council (CSC), and a research consortium including BG Group, BP, DONG, RWE Dea, Petrochina, Statoil and Tullow Oil. The authors thank all the many people associated with the deepwater research group at the University of Aberdeen, for their contributions to the mapping, description and interpretation of the study area, which provide the basis for this manuscript. Coding of the sedimentary logs and Markov chain analysis of coded logs were carried out respectively using the Matlab code (https://csdms.colorado.edu/wiki/Model:OptimalCycleID) of Peter Burgess, and by the program phpSediStat (http://phpsedistat.sourceforge.net/index.html) of Staňová Sidónia, Soták Ján and Hudec Norbert. We thank the reviewers …….. and ……. for their helpful and constructive comments. | en |
| dc.description.status | Peer reviewed | en |
| dc.format.extent | 18 | |
| dc.format.extent | 20719810 | |
| dc.identifier | 112527781 | |
| dc.identifier | ea4b2e88-6def-4a05-b33c-cd203d99353d | |
| dc.identifier | 85042472006 | |
| dc.identifier.citation | Li, P, Kneller, B C, Thompson, P, Bozetti, G & Dos Santos, T 2018, 'Architectural and facies organization of slope channel fills : Upper Cretaceous Rosario Formation, Baja California, Mexico', Marine and Petroleum Geology, vol. 92, pp. 632-649. https://doi.org/10.1016/j.marpetgeo.2017.11.026 | en |
| dc.identifier.doi | 10.1016/j.marpetgeo.2017.11.026 | |
| dc.identifier.issn | 0264-8172 | |
| dc.identifier.uri | http://hdl.handle.net/2164/11529 | |
| dc.identifier.vol | 92 | en |
| dc.language.iso | eng | |
| dc.relation.ispartof | Marine and Petroleum Geology | en |
| dc.subject | Turbidite | en |
| dc.subject | Slope channel | en |
| dc.subject | Architecture organization | en |
| dc.subject | Vertical facies trend | en |
| dc.subject | Deep-water outcrop analogue | en |
| dc.subject | QE Geology | en |
| dc.subject | Supplementary Data | en |
| dc.subject | http://dx.doi.org/10.1016/j.marpetgeo.2017.11.026 | en |
| dc.subject.lcc | QE | en |
| dc.title | Architectural and facies organization of slope channel fills : Upper Cretaceous Rosario Formation, Baja California, Mexico | en |
| dc.type | Journal article | en |