Zobrazeno 1 - 10
of 10
pro vyhledávání: '"Fabio Lapponi"'
Autor:
Mar Moragas, Vinyet Baqués, Juan Diego Martín-Martín, Ian Sharp, Fabio Lapponi, David Hunt, Michael Zeller, Jaume Vergés, Grégoire Messager, Laurent Gindre-Chanu, Roger Swart, Vladimir Machado
Publikováno v:
Marine and Petroleum Geology
The Aptian Pre-Salt sedimentary succession cropping out in Cangulo palaeovalley onshore Namibe Basin (Angola) was studied by a combination of field and analytical techniques to constrain the sedimentary and diagenetic evolution of the uppermost sag s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2dec0843ef18b0ad2253711dad09b228
https://hdl.handle.net/11250/3075545
https://hdl.handle.net/11250/3075545
Autor:
A. Waldum, P.H. Vieira de Luca, D. Hunt, L. Loures, E. Castro, G. Nery Camargo, G. McQueen, O.P. Wennberg, A.S. Chandler, Fabio Lapponi
Publikováno v:
Petroleum Geoscience. 27
Natural open fractures are present in sidewall cores and in whole-core samples from pre-salt reservoirs in the licence block BM-C-33 in the Campos Basin, Brazil. Open fractures are also observed in borehole image logs, and fracture densities are in g
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f50bf7f60a99d967e14b1b8c1b4bf4d6
https://doi.org/10.1144/petgeo2020-125
https://doi.org/10.1144/petgeo2020-125
Autor:
A. Waldum, P.H. Vieira de Luca, D. Hunt, A.S. Chandler, Fabio Lapponi, O.P. Wennberg, G. McQueen
Publikováno v:
First EAGE Workshop on Pre-Salt Reservoir: from Exploration to Production.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d7ba979b4fb3adf4ac96e6d67c46c026
https://doi.org/10.3997/2214-4609.201982010
https://doi.org/10.3997/2214-4609.201982010
Publikováno v:
Sedimentology. 61:411-443
Burial hydrothermal dolomitization is a common diagenetic modification in sedimentary basins with implications for oil and gas reservoir performance. Outcrop analogues represent an easily accessible source of data to refine the genetic models and ass
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cacf99ec27676ed3908b555bcf43fe06
https://doi.org/10.1111/sed.12060
https://doi.org/10.1111/sed.12060
Deformation bands in chalk, examples from the Shetland Group of the Oseberg Field, North Sea, Norway
Autor:
Jon R. Ineson, Ali Jahanpanah, Brita Graham Wall, Paul Gillespie, Giulio Casini, Fabio Lapponi, O.P. Wennberg
Publikováno v:
Journal of Structural Geology. 56:103-117
Deformation bands are described in detail for the first time in carbonate rock from the subsurface and in chalk from the North Sea. The samples are from 2200 to 2300 m below sea level, in upper Maastrichtian to Danian chalk in the Oseberg Field. The
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c028010f59ad285118827ce6f8c05e48
https://doi.org/10.1016/j.jsg.2013.09.005
https://doi.org/10.1016/j.jsg.2013.09.005
Autor:
Baqués, Vinyet, Moragas, Mar, Fabio, Lapponi, Zeller, Michael, Hunt, David, Casciello, Emilio, Vergés, Jaume, Cruz, Israel, Messager, G., Sharp, Ian, Higgins, S., Freitag, Ulrike, Ferreira, Herrcinda, Machado, Vladamir
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
instname
AAPG 2016 Annual Convention & Exhibition Occured on 19-22 June 2016 Calgary, Canada
The Cangulo Fm., exposed onshore within the Namibe Basin of Angola, belongs to the Pre-Salt succession, characterized by fluvial to marginal marine sediments dep
The Cangulo Fm., exposed onshore within the Namibe Basin of Angola, belongs to the Pre-Salt succession, characterized by fluvial to marginal marine sediments dep
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::0fdd1ef16e2c1f665d29c20335cf3fcc
http://hdl.handle.net/10261/229778
http://hdl.handle.net/10261/229778
Autor:
David Hunt, Ian R. Sharp, Naiara Fernandez, I. Romaire, Giulio Casini, Fabio Lapponi, Wolfgang Blendinger
Publikováno v:
Petroleum Geoscience. 17:283-307
Outcrop data derived from fieldwork, remote sensing satellite and LiDAR-derived 3D models were used to build an integrated dual porosity-permeability static reservoir model which captured stratigraphic, diagenetic and structural heterogeneities. The
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9318cf3e17266ebf2f66512e01547330
https://doi.org/10.1144/1354-079310-040
https://doi.org/10.1144/1354-079310-040
Publikováno v:
Terra Nova. 19:440-444
The origin of many dolomites is still a matter of debate because of many possible chemical and hydrological conditions of formation. Fluid inclusion studies have been applied in order to improve knowledge about paleofluids responsible for the precipi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::99f273def37de16bf4781356c4af9b33
https://doi.org/10.1111/j.1365-3121.2007.00769.x
https://doi.org/10.1111/j.1365-3121.2007.00769.x
Publikováno v:
Economic Geology. 97:1815-1827
Zinc-lead deposits hosted by Lower Cambrian carbonate rocks near Huayuan in the Hunan-Guizhou orogenic belt, southern China, have been studied by means of Pb and Sr isotopes. The deposits are characterized by two mineralization stages: (1) a main eco
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::17e4ce5efbe846588d2f4e391e7c9580
https://doi.org/10.2113/gsecongeo.97.8.1815
https://doi.org/10.2113/gsecongeo.97.8.1815
Autor:
Ian R. Sharp, A. Amilibia Cabeza, W. Blendingen, Giulio Casini, T. Needham, J. Garland, Paul Gillespie, T. L. Scarrott, D. Hunt, Fabio Lapponi, Rudy Swennen
Publikováno v:
Proceedings.
Late burial dolomite of hydrothermal origin replaces Cretaceous carbonate shelf sediments of Albian to Turonian age (Sarvak Formation) in the NW closure of the Anaran Anticline, Zagros Mountains, Simply Folded Belt, Iran. The outcrops, spectacularly
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5b254f987641e0b72fbcc9f83df8796c
https://doi.org/10.3997/2214-4609.20145358
https://doi.org/10.3997/2214-4609.20145358