Zobrazeno 1 - 2
of 2
pro vyhledávání: '"ddc:552.3"'
Autor:
Khaksar, Tayebeh, Rashidnejad‐Omran, Nematollah, Li, Shuang‐Qing, Song, Shu‐Guang, Kananian, Ali, Chen, Fukun, Li, Su, 1 Department of Geology, Faculty of Basic Sciences Tarbiat Modares University Tehran Iran, 3 Department of Geology School of Earth and Space Sciences, Peking University Beijing China, 4 School of Geology College of Science, University of Tehran Tehran Iran, 5 Department of Geochemistry and Environmental sciences School of Earth and Space Sciences University of Science and Technology of China Hefei China, 6 State Key Laboratory of Geological Processes and Mineral Resources Institute of Earth Science, Chinese University of Geosciences Beijing China
The Ghohroud granitoids (GG), containing mafic microgranular enclaves (MMEs) are located in the central part of the Urumieh‐Dokhtar Magmatic Arc (UDMA) in central Iran. They are associated with the subduction‐related magmatism in the Alpine‐Him
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7b0e323cded3e580aedefbde08c3e0f0
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/10166
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/10166
Autor:
Aspiotis, S., Jung, S., Hauff, F., Romer, R. L., Mineralogisch-Petrographisches Institut, Universität Hamburg, Hamburg, Germany, GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel, Kiel, Germany, Deutsches GeoForschungsZentrum GFZ, Potsdam, Germany
Publikováno v:
International Journal of Earth Sciences
The late-tectonic 511.4 ± 0.6 Ma-old Nomatsaus intrusion (Donkerhoek batholith, Damara orogen, Namibia) consists of moderately peraluminous, magnesian, calc-alkalic to calcic granites similar to I-type granites worldwide. Major and trace-element var
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::830058601226b9ae687fa45579a155ed
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5006815
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5006815