Instituto Geológico y Minero de España

LogoSistema de información documental - SID

 

 

 

Resultados de la consulta :
Instituto Geológico y Minero de España
 Registros del al 10 de 48 encontrados

1.-  Basement depths in the Parecis Basin (Amazon) with receiver functions from small local earthquakes in the Porto dos Gauchos seismic zone
Elsevier; Oxford; GBR; United Kingdom, 2011
Ver registro

2.-  Crustal thickness and structure of Precambrian South America from receiver function analysis
American Geophysical Union; Washington, DC; USA; United States, 2006
AGU 2006 fall meeting
Ver registro

3.-  Crustal thickness map of Brazil; data compilation and main features
Elsevier; Oxford; GBR; United Kingdom, 2013
Ver registro

4.-  CRUSTAL THICKNESSES IN SOUTHEASTERN BRAZILIAN SHIELD BY RECEIVER FUNCTION ANALYSIS; IMPLICATIONS FOR ISOSTATIC COMPENSATION
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2002
Ver registro

5.-  FIRST SEISMIC EVIDENCES FOR ANOMALIES RELATED TO THE TRINDADE PLUME IN SE AND CENTRAL BRAZIL
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2002
AGU 2002 FALL MEETING
Ver registro

6.-  FOCAL MECHANISMS OF SMALL EARTHQUAKES IN THE SOUTHEASTERN BRAZILIAN SHIELD; A TEST OF STRESS MODELS OF THE SOUTH AMERICAN PLATE
BLACKWELL SCIENTIFIC; OXFORD; GBR; UNITED KINGDOM, 1998
Ver registro

7.-  FOSSIL PLUMES, FLOOD BASALTS, AND EVIDENCE FOR COHERENT FLOW OF LITHOSPHERE AND UPPER MANTLE BENEATH SOUTH AMERICA
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 1995
AGU 1995 SPRING MEETING
Ver registro

8.-  Genetic algorithm inversion of the average 1D crustal structure using local and regional earthquakes
Elsevier; Amsterdam; NLD; Netherlands, 2011
Ver registro

9.-  GENETIC ALGORITHM; FINITE ELEMENT INVERSION OF INTRAPLATE STRESS FIELD IN BRAZIL
IUGG; [LOCATION VARIES]; III; INTERNATIONAL, 1999
IUGG 99; ABSTRACTS
Ver registro

10.-  GENETIC ALGORITHM-FINITE ELEMENT INVERSION OF STRESS FIELD IN BRAZIL
ZHONGGUO WULIXUE HUI; BEIJING; CHN; CHINA, 2000
Ver registro


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