Instituto Geológico y Minero de España

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Resultados de la consulta :
Instituto Geológico y Minero de España
 Registros del al 7 de 7 encontrados

1.-  Lower Ordovician carbonate platform (La Silla Formation), eastern Precordillera, Argentina
Geological Association of Canada; Waterloo, ON; CAN; Canada, 2008
Geological Association of Canada, Mineralogical Association of Canada; joint annual meeting; abstracts--Association geologique du Canada, Association mineralogique du Canada; congres annuel conjoint; recueil des resumes
Ver registro

2.-  MIDDLE CAMBRIAN TRILOBITES OF LA LAJA FORMATION, WESTERN ARGENTINA
INSTITUTO GEOLOGICO Y MINERO DE ESPAÑA;MADRID;ESP, 2008
ADVANCES IN TRILOBITES RESEARCH: FOURTH INTERNATIONAL TRILOBITE CONFERENCE, TOLEDO, JUNE, 16-14, 2008
Ver registro

3.-  MOLAR-TOOTH STRUCTURE: FORMATION BY EARTHQUAKE-INDUCED SHRINKAGE, AND HOW IT AIDS TECTONIC, PALEOCEANOGRAPHIC AND PALEOBATHYMETRIC RECONSTRUCTION OF PRECAMBRIAN BASINS

ALICANTE: UNIV. ALICANTE, 1998
15TH. INTERNATIONAL SEDIMENTOLOGICAL CONGRESS. ABSTRACTS
Ver registro

4.-  STROMATOPOROID PATCH REEFS FROM THE FAMENNIAN (UPPER DEVONIAN) PALLISER FORMATION, WEST-CENTRAL ALBERTA, CANADA

ALICANTE: UNIV. ALICANTE, 1998
15TH. INTERNATIONAL SEDIMENTOLOGICAL CONGRESS. ABSTRACTS
Ver registro

5.-  TAPHONOMY OF MIDDLE CAMBRIAN TRILOBITES: DISTINGUISHING TSUNAMIS FROM STORMS IN LA LAJA FORMATION OF WESTERN ARGENTINA
INSTITUTO GEOLOGICO Y MINERO DE ESPAÑA;MADRID;ESP, 2008
ADVANCES IN TRILOBITES RESEARCH: FOURTH INTERNATIONAL TRILOBITE CONFERENCE, TOLEDO, JUNE, 16-14, 2008
Ver registro

6.-  TRILOBITE-BASED BIOESTRATIGRAPHIC MODEL (BIOFACIES AND BIOZONATION) FOR THE MIDDLE CAMBRIAN CARBONATE PLATFORM OF THE ARGENTINE PRECORDILLERA
2008
LOWER PALEOZOIC BIOSTRATIGRAPHY OF SOUTH AMERICA: NEW CONTRIBUTIONS AND ADVANCES
Ver registro

7.-  Tsunamis in a stormy sea; Middle Cambrian limestones of western Argentina
Geological Association of Canada; Waterloo, ON; CAN; Canada, 2006
GAC-MAC annual meeting; abstracts--AGC-AMC congres annuel; resumes
Ver registro


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