Registros del 1 al 5 de 5 encontrados |
![](./images/clear.gif) 1.- Behavior of fluid-mobile elements in serpentines from abyssal to subduction environments; examples from Cuba and Dominican Republic
Elsevier; Amsterdam; NLD; Netherlands, 2012
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![](./images/clear.gif) 2.- ENRICHMENT OF HFSE IN CHLORITE-HARZBURGITE PRODUCED BY HIGH-PRESSURE DEHYDRATION OF ANTIGORITE-SERPENTINITE; IMPLICATIONS FOR SUBDUCTION MAGMATISM
AMERICAN GEOPHYSICAL UNION AND THE GEOCHEMICAL SOCIETY;; USA; UNITED STATES, 2005
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![](./images/clear.gif) 3.- Genetical relationships between cumulate gabbros and volcanic rocks in the Mayari-Baracoa ophiolitic belt (eastern Cuba)
[International Geological Congress]; [location varies]; III; International, 2004
Italia 2004; 32nd international geological congress; abstracts
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![](./images/clear.gif) 4.- New geochemical data on peridotites from Mayari-Cristal and Moa-Baracoa ophiolite massifs (eastern Cuba)
[International Geological Congress]; [location varies]; III; International, 2004
Italia 2004; 32nd international geological congress; abstracts
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![](./images/clear.gif) 5.- Serpentinites act as sponges for fluid-mobile elements in abyssal and subduction zone environments
Wiley-Blackwell; Oxford; GBR; United Kingdom, 2011
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