Zobrazeno 1 - 8
of 8
pro vyhledávání: '"J. Lincoln Foreman"'
Autor:
J. Lincoln Foreman, Thomas A. Jones
Publikováno v:
Computers & Geosciences. 29:1033-1044
Object-based (or Boolean) methods are used to create channels, bars, splays, or other features to model the distribution of facies in a reservoir. Geologic objects and their facies subsequently are used as templates to control the distribution of pet
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::483ea1db9334152b2e826e05887c7653
https://doi.org/10.1016/s0098-3004(03)00100-6
https://doi.org/10.1016/s0098-3004(03)00100-6
Autor:
J. Lincoln Foreman, Steven G. Driese
Publikováno v:
Ichnos. 1:207-219
Traces interpreted as Skolithos sp. in a Glossifungites ichnofacies occur in the upper part of the Beans Gap Claystone paleosol, in association with a Late Ordovician marine erosional surface. Paleosol color and whole‐rock chemistry are distinctly
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9050543cb915cad012646ce73fbaf52d
https://doi.org/10.1080/10420949109386353
https://doi.org/10.1080/10420949109386353
Autor:
William M. Dunne, J. Lincoln Foreman
Publikováno v:
Journal of Structural Geology. 13:1173-1183
The Nolichucky Shale in the Whiteoak Mountain thrust sheet of the southern Appalachian foreland contains four coeval bed-normal calcite vein sets that trended 015°, 055°, 090° and 320° before thrusting. The pretectonic veins were displaced by syn
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::481e6cdc4192a9c1172ac0b1d53798e5
https://doi.org/10.1016/0191-8141(91)90076-u
https://doi.org/10.1016/0191-8141(91)90076-u
Autor:
G. N. Jensen, David C. Jennette, Frank J. Goulding, Morgan D. Sullivan, J. Lincoln Foreman, David Stern
The situation presented at the Diana field in the western Gulf of Mexico is a common one in exploration and early development: a hydrocarbon reservoir expressed by a single-cycle seismic event and limited appraisal wells spaced thousands of feet apar
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c14dd79150d4f321ed3f0e4490b7fbe6
https://doi.org/10.1306/m80924c11
https://doi.org/10.1306/m80924c11
Autor:
J. Lincoln Foreman, Steven G. Driese
Publikováno v:
SEPM Journal of Sedimentary Research. 62
Claystone paleosols with abundant vertic features occur in Upper Ordovician (Ashgillian) red beds of the Juniata Formation in the southern Appalachians. The Beans Gap Claystone paleosol formed during Late Ordovician pedogenesis of estuarine and upper
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fee454dc646f9dabc715d346df70067e
https://doi.org/10.1306/d4267893-2b26-11d7-8648000102c1865d
https://doi.org/10.1306/d4267893-2b26-11d7-8648000102c1865d
Publikováno v:
SEPM Journal of Sedimentary Research. 62
Paleosols with vertic (Vertisol-like) features occur in repetitively stacked fining-upward sequences bounded by marine erosional surfaces in the Bloomsburg Formation (Ludlovian to Pridolian) of central Pennsylvania. Paleosol development was strongly
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::65dec4adade327d4d44f2ba84c6d6578
https://doi.org/10.1306/d42679ec-2b26-11d7-8648000102c1865d
https://doi.org/10.1306/d42679ec-2b26-11d7-8648000102c1865d
Autor:
Driese, Steven G., Foreman, J. Lincoln
Publikováno v:
Ichnos; Aug1991, Vol. 1 Issue 3, p207-219, 13p
Publikováno v:
Carbonates & Evaporites; Sep1990, Vol. 5 Issue 2, p141-152, 12p