| Registros del 1 al 10 de 1749 encontrados |
 1.- "BEACHROKS" HOLOCENOS DE LA ISLA DE LA REUNION, OCEANO INDICO
1997
Ver registro
 2.- (super 87) Sr/ (super 86) Sr ratios in inoceramids (Bivalvia) and carbonate matrix as indicators of differential diagenesis during burial; early Maastrichtian Bay of Biscay sections (Spain and France); potential use for chemostratigraphy?
Elsevier;; GBR; United Kingdom, 2008
Ver registro
 3.- 1.LA DIAGENESIS EN LA DOLOMITA Y MAGNESITA DE ASTURRETA(EUGUI,NAVARRA): UN PROBLEMA POR ESTUDIAR.,
1968
Ver registro
 4.- 3-D DELINEATION OF THE STRUCTURAL AND STRATIGRAPHIC CONTROLS ON HYDROCARBON ACCUMULATION IN THE SENAL PICADA BLOCK, NEUQUEN BASIN, ARGENTINA
AMERICAN ASSOCIATION OF PETROLEUM GEOLOGISTS; TULSA, OK; USA; UNITED STATES, 1998
AAPG INTERNATIONAL CONFERENCE AND EXHIBITION; ABSTRACTS
Ver registro
 5.- 3-D static and dynamic modeling of a carbonate reservoir; the Lower Cretaceous La Tosca Unit (Huitrin Formation, Neuquen Basin, Argentina)
American Association of Petroleum Geologists and Society for Sedimentary Geology; Tulsa, OK; USA; Un, 2012
2012 AAPG annual convention & exhibition; abstracts volume
Ver registro
 6.- A 2-D PETROLEUM SYSTEM MODELING FOR COMPRESSIVE AND EXTENSIONAL TERRAINS
AMERICAN ASSOCIATION OF PETROLEUM GEOLOGISTS AND SOCIETY OF ECONOMIC PALEONTOLOGISTS AND MINERALOGIS, 2003
2003 AAPG ANNUAL CONVENTION WITH SEPM
Ver registro
 7.- A BENTONITE BED IN THE ACEGUA (RS, BRAZIL) AND MELO (URUGUAY) AREAS; A HIGHLY CRYSTALLIZED MONTMORILLONITE
ELSEVIER; OXFORD; GBR; UNITED KINGDOM, 2003
Ver registro
 8.- A COMPARATIVE STUDY OF FOSSIL AND EXTANT ALGAENANS USING RUTHENIUM TETROXIDE DEGRADATION
PERGAMON; OXFORD; III; INTERNATIONAL, 2000
Ver registro
 9.- A COMPARATIVE STUDY OF THE DIAGENESIS IN DIAPIR INFLUENCED REEF ATOLLS AND A FAULT BLOCK REEF PLATFORM IN THE LATE ALBIAN OF THE VASCO-CANTABRIAN BASIN (NORTHERN SPAIN)

BERLIN: SPRINGER, 1986
REEF DIAGENESIS
Ver registro
 10.- A DIAGENESIS TO METAMORPHISM TRANSITION IN THE HERCYNIAN OF NORTH WEST SPAIN
1985
Ver registro
|
|
|