Zobrazeno 1 - 10
of 69
pro vyhledávání: '"Clyde H. Moore"'
Autor:
Clyde H. Moore, William J. Wade
The 2nd Edition of Carbonate Reservoirs aims to educate graduate students and industry professionals on the complexities of porosity evolution in carbonate reservoirs. In the intervening 12 years since the first edition, there have been numerous stud
Autor:
William J. Wade, Clyde H. Moore
The biological influence over the origin, distribution, composition, texture, and mineralogy of carbonate sediments is stressed. Environmental factors such as light, temperature, and water depth directly affect these biological processes. Abiotic car
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c402d07a2dd0c71b955d2e20ad57c0d1
https://doi.org/10.1016/b978-0-444-53831-4.00001-x
https://doi.org/10.1016/b978-0-444-53831-4.00001-x
Autor:
Clyde H. Moore, William J. Wade
Sequence stratigraphic principals can be applied to carbonate rock sequences. Typical tropical shallow-water carbonate shelves lead to sequence boundary exposure across carbonate platforms, and carbonate deep water deposits during highstands. Rapid c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1854f4f9208c5fdb6b9d44a4aab09651
https://doi.org/10.1016/b978-0-444-53831-4.00002-1
https://doi.org/10.1016/b978-0-444-53831-4.00002-1
Autor:
William J. Wade, Clyde H. Moore
Three economically important case histories serve as illustrations of the integration of analyses of depositional environments, sequence stratigraphic architecture, and porosity evolution during diagenesis, as a means of maximizing effectiveness of r
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fe16716ebaa0850c59d65ed51cfeaddf
https://doi.org/10.1016/b978-0-444-53831-4.00012-4
https://doi.org/10.1016/b978-0-444-53831-4.00012-4
Autor:
Clyde H. Moore, William J. Wade
Phanerozoic Global tectonic cycles (rifting of supercontinents, drifting and disassembly, closure and assembly) have a major impact of the development of the carbonate system. Volcanism during rifting affects global climate, leading to icehouse and g
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::295224a8b5e9a7bca3003c38eea575ee
https://doi.org/10.1016/b978-0-444-53831-4.00003-3
https://doi.org/10.1016/b978-0-444-53831-4.00003-3
Autor:
William J. Wade, Clyde H. Moore
The porosity of carbonates as compared to sandstones is vastly more complex with simple intergrain porosity dominates sandstones while carbonates commonly exhibit complex secondary pore systems that may evolve during burial. Initial porosity of carbo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::42918cb9f4fa926d518e175233ad17a2
https://doi.org/10.1016/b978-0-444-53831-4.00004-5
https://doi.org/10.1016/b978-0-444-53831-4.00004-5
Autor:
Clyde H. Moore, William J. Wade
Shallow-marine carbonate sequences commonly undergo exposure to meteoric waters. These waters are chemically aggressive toward sedimentary carbonate minerals, capable of rapidly dissolving grains and generating secondary porosity. The carbonate deriv
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::20727514de47e8ccd4cc0b585b173b86
https://doi.org/10.1016/b978-0-444-53831-4.00008-2
https://doi.org/10.1016/b978-0-444-53831-4.00008-2
Autor:
William J. Wade, Clyde H. Moore
The overarching diagenetic drive during progressive burial of carbonate rocks is toward the loss of porosity through mechanical and chemical compaction (the latter consisting of pressure solution plus related cementation). The passive margin diagenet
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9b3b8bb2b8926930f0898d0991984c7a
https://doi.org/10.1016/b978-0-444-53831-4.00010-0
https://doi.org/10.1016/b978-0-444-53831-4.00010-0
Autor:
Clyde H. Moore, William J. Wade
Carbonate reservoirs are prone to natural fracturing. Fractures can act as enhanced permeability pathways, which may increase, decrease, or complicate reservoir production and development; healed fractures contribute to reservoir compartmentalization
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f35857f92476213a5aef4cf49f9645ec
https://doi.org/10.1016/b978-0-444-53831-4.00011-2
https://doi.org/10.1016/b978-0-444-53831-4.00011-2
Autor:
William J. Wade, Clyde H. Moore
The three diagenetic realms in which porosity modifications (e.g., dissolution, cementation, compaction) take place are the marine, meteoric, and subsurface environments. The meteoric environment—with its dilute waters, easy access to CO2, and wide
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a4543e103e1ded3bb543491e07ba0b1a
https://doi.org/10.1016/b978-0-444-53831-4.00005-7
https://doi.org/10.1016/b978-0-444-53831-4.00005-7