Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Abdul Razak Damit"'
Autor:
Daniel S. Collins, Alexandros Avdis, Peter A. Allison, Howard D. Johnson, Jon Hill, Matthew D. Piggott, Meor H. Amir Hassan, Abdul Razak Damit
Publikováno v:
Nature Communications, Vol 8, Iss 1, Pp 1-12 (2017)
Mangroves are important carbon-rich biomes, but their long-term impact on the global carbon cycle is relatively unknown. Here, the authors show that the Oligo–Miocene mangroves in the South China Sea stored in excess of 4,000 Gt, demonstrating the
Externí odkaz:
https://doaj.org/article/ea1ef380a7bc4e33a5d1ca59b15e2f6f
Publikováno v:
Journal of Sedimentary Research. 88:399-430
This evaluation of the Miocene–Modern Baram Delta Province (BDP) depositional system provides: (1) a rare case study of outcrop observations that can be directly compared with a closely comparable and geographically adjacent modern analogue; (2) ne
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0b366e9f2cfdbba44794e4519637b565
https://doi.org/10.2110/jsr.2018.19
https://doi.org/10.2110/jsr.2018.19
Autor:
Howard D. Johnson, Peter A. Allison, Alexandros Avdis, Abdul Razak Damit, Matthew D. Piggott, Daniel S. Collins, Meor Hakif Amir Hassan, Jon Hill
Publikováno v:
Nature Communications, Vol 8, Iss 1, Pp 1-12 (2017)
Nature Communications
Nature Communications
Modern mangroves are among the most carbon-rich biomes on Earth, but their long-term (≥106 years) impact on the global carbon cycle is unknown. The extent, productivity and preservation of mangroves are controlled by the interplay of tectonics, glo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4148d75fc8d63a025703dce020d36e79
http://hdl.handle.net/10044/1/45631
http://hdl.handle.net/10044/1/45631
Publikováno v:
Basin Research. 22:236-247
The Baram Delta System, Brunei, NW Borneo, is a Tertiary delta system located on an active continental margin. Delta top regions in many Tertiary delta systems (e.g. Niger Delta) are thought to exhibit a normal-fault stress regime and margin-parallel
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::43ea4633048f09f1121bf995d55a1c9f
https://doi.org/10.1111/j.1365-2117.2009.00407.x
https://doi.org/10.1111/j.1365-2117.2009.00407.x
Autor:
Abdul Razak Damit, Richard R. Hillis, Christopher K. Morley, Richard E. Swarbrick, Mark Tingay
Publikováno v:
AAPG Bulletin. 93:51-74
Accurate pore-pressure prediction is critical in hydrocarbon exploration and is especially important in the rapidly deposited Tertiary Baram Delta province where all economic fields exhibit overpressures, commonly of high magnitude and with narrow tr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e4ed46592c06bfa8715ed16a1c29783f
https://doi.org/10.1306/08080808016
https://doi.org/10.1306/08080808016
Present-day stress and neotectonics of Brunei: Implications for petroleum exploration and production
Autor:
Abdul Razak Damit, Richard E. Swarbrick, Richard R. Hillis, Christopher K. Morley, Mark Tingay, Rosalind King
Publikováno v:
AAPG Bulletin. 93:75-100
The present-day state of stress in Tertiary deltas is poorly understood but vital for a range of applications such as wellbore stability and fracture stimulation. The Tertiary Baram Delta province, Brunei, exhibits a range of contemporary stress valu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fd44cf637106afee445ad4980476c012
https://doi.org/10.1306/08080808031
https://doi.org/10.1306/08080808031
Autor:
Peter A. Allison, Abdul Razak Damit, Meor Hakif Amir Hassan, Wan Hasiah Abdullah, Howard D. Johnson
Publikováno v:
PGCE 2009.
The Early Miocene (Cycles I-II) of the southwestern Sarawak Basin (Tatau-Balingian-Tinjar Provinces) is comprised of thick (>6 km), vertically stacked successions of alluvial plain, coastal plain, coastal and offshore depositional systems. The lower
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c040b4d8d91d5ca29708c6dd47e53cde
https://doi.org/10.3997/2214-4609-pdb.254.p18
https://doi.org/10.3997/2214-4609-pdb.254.p18
Autor:
Richard E. Swarbrick, Abdul Razak Damit, Richard R. Hillis, Christopher K. Morley, Mark Tingay
Publikováno v:
Geology. 35:1023
Overpressures in sedimentary basins are commonly assumed to be the result of two distinct and separate mechanisms: disequilibrium compaction and fluid expansion. However, the potential for overpressures to be redistributed or transferred to other pre
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4eedc5c3322a78a62ee45d56711b9566
https://doi.org/10.1130/g23906a.1
https://doi.org/10.1130/g23906a.1