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Garnet peridotite found in the Greater Antilles
Author(s) -
Abbott Richard N.,
Draper Grenville,
Keshav Shantanu
Publication year - 2001
Publication title -
eos, transactions american geophysical union
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.316
H-Index - 86
eISSN - 2324-9250
pISSN - 0096-3941
DOI - 10.1029/01eo00236
Subject(s) - peridotite , geology , terrane , peninsula , geochemistry , mantle (geology) , geography , seismology , tectonics , archaeology
Although Alpine peridotites are relatively common in collisional orogenic zones, garnet‐bearing peridotites are rare and only associated with high pressure/ultra‐high pressure or temperature (HP/UHP or T) terranes [ Brueckner and Medaris , 2000; Medaris , 1999]. Until recently all reported occurrences of Alpine‐type garnet peridotites and HP/UHP terranes were in Eurasia and Africa, with one occurrence in the Seward Peninsula, Alaska [ Till , 1981; Lieberman and Till , 1987]. Now a new Alpine‐type garnet peridotite locality has been discovered in the Caribbean island of Hispaniola. This discovery is the second of its kind in the Americas.

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