Open AccessGRANITOID PETROLOGY OF HAI VAN MASSIF
Author(s) -
Phuc Duc Le
Publication year - 2009
Publication title -
khoa học công nghệ
Language(s) - English
Resource type - Journals
ISSN - 1859-0128
DOI - 10.32508/stdj.v12i5.2243
Subject(s) - massif , geology , geochemistry , biotite , mantle (geology) , crust , homogeneous , source rock , petrology , geomorphology , paleontology , quartz , physics , thermodynamics , structural basin
The granitoid formations of Hai Van massif with petrographical components consist of biotite granite, two mica granite. Chemical components of rocks are: SiO2: 69,34=73,92%, Na2O+KO: 6,11-8,11%, K2O/Na20>1. Content of Ba, Sr is low but Rb is higher. From results of Nd-Sm isotopic analysic shows that they are nearly same with stable crust material. Age of source region formation is 1,33 billion years (model of homogeneous chondrite source region), or 1,95 billion years (model of poor mantle source region). U-Pb isotopic age: 241,9+ 2 and 241,4+2.1 million years.