Zobrazeno 1 - 10
of 11
pro vyhledávání: '"Gregory Frébourg"'
Geologic Modeling of Eagle Ford Facies Continuity Based on Outcrop Images and Depositional Processes
Publikováno v:
SPE Journal. 23:1359-1371
Summary Geologic modeling of mudrock reservoirs is complicated by the presence of multiscale heterogeneities and lithofacies lateral discontinuity. The resolution of wireline logs is also too low to capture many small-scale heterogeneities that affec
Publikováno v:
AAPG Bulletin. 100:657-682
A detailed sedimentological study of the middle Eagle Ford/Boquillas (outcrop analog of subsurface producing strata) units was conducted on numerous roads cut along US Highway 90 in Val Verde County and on outcrops in Big Bend National Park, Brewster
The subsurface Upper Jurassic Haynesville and Bossier Formations comprise three facies associations along the eastern slope of the Gilmer Platform. The lower Haynesville facies association consists of three facies produced by mass-wasting processes:
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::944f6ef4cd285b00391a2b2fcb50a7aa
https://doi.org/10.1306/13441844m1053599
https://doi.org/10.1306/13441844m1053599
Autor:
Gregory Frébourg, Ursula Hammes
Publikováno v:
Marine and Petroleum Geology. 31:8-26
Upper Jurassic Haynesville and Bossier shale-gas plays of the northwestern Gulf of Mexico (GOM) Basin produce from organic-rich, marine transgressive to highstand mudrocks within mixed carbonate-clastic depositional systems. Modern wireline-log suite
Publikováno v:
Sedimentology. 59:1409-1425
An outcrop study of uplifted marine terraces provides information on the climate of past sea-level maxima, supplementing existing palaeoclimatological archives. The western coast of the Akamas Peninsula shows several uplifted and intricately stacked
Publikováno v:
Journal of Petroleum Geology, Vol. 33, No 2 (2010) pp. 141-154
A laterally continuous, 3m thick oolitic grainstone has been studied in cores from two wells from the South Pars field (offshore Iran). This high porosity but low permeability interval occurs at the top of the gas-bearing succession in the Permian Up
Publikováno v:
Sedimentary Geology
Sedimentary Geology, Vol. 224, No 1-4 (2010) pp. 38-48
Sedimentary Geology, Vol. 224, No 1-4 (2010) pp. 38-48
A high-energy deposit cuts through the early Holocene eolianites of the Sidi Salem Formation which forms a ridge along the southeastern coast of Tunisia. The sedimentary structures as well as the paleo-altitude and paleo-location of the outcrop state
Publikováno v:
Facies, Vol. 54, No 2 (2008) pp. 175-191
Carbonate eolian dunes can form huge sand bodies along the coasts but are seldom described in the pre-Quaternary record. The study of more than 600 thin-sections collected in present-day, Holocene and Pleistocene dunes from Sardinia, Crete, Cyprus, T
Autor:
Gregory Frébourg, Isabelle Billeaud, Bernadette Tessier, Eric Jean Davaud, Benjamin Livas, Bruno Caline, Dominique Laurier, Cecile Pabian-Goyheneche, Claude-Alain Hasler
Publikováno v:
Geological Society-Special Publications, Vol. 388 (2013)
The southern coast of the Arabian Gulf is considered a good example of an arid carbonate depositional system. The objective of this field investigation is to better elucidate the dynamic controls on the character and pattern of the depositional belts
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f3cd4af9e5cbec6d2baa8e02bb7ecef0
https://archive-ouverte.unige.ch/unige:33219
https://archive-ouverte.unige.ch/unige:33219
Publikováno v:
Facies, Vol. 58, No 4 (2012) pp. 509-522
Facies
Facies
Although eolian deposits are known to record the dominant winds, secondary conditions such as wind reversals during wintertime can also be observed in the petrographic composition and facies succession. Thus, eolian deposits are used here as a local
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::da9a162e3a6192b9358f81313dca7b88
https://archive-ouverte.unige.ch/unige:27719
https://archive-ouverte.unige.ch/unige:27719