Mineral Chemistry and Geochemistry of Volcanic Rocks in The North of Pasinler (Erzurum)

In the north of Pasinler (Erzurum), Upper Miocene-Pliocene volcanic rocks crop out. These volcanites are composed of basaltic andesite, andesite, dacite, rhyolite lavas and rhyolitic pyroclastics. The rocks show porphyritic, microlitic porphyritic, hyalo-microlitic porphyritic, vitrophyric, glomerop...

Full description

Bibliographic Details
Main Authors: Oktay KILIÇ, Hüseyin KURT, Kürşad ASAN, Gürsel KANSUN
Format: Article
Language:English
Published: Pamukkale University 2009-02-01
Series:Pamukkale University Journal of Engineering Sciences
Subjects:
Online Access:http://dergipark.ulakbim.gov.tr/pajes/article/view/5000088821
_version_ 1797908653774209024
author Oktay KILIÇ
Hüseyin KURT
Kürşad ASAN
Gürsel KANSUN
author_facet Oktay KILIÇ
Hüseyin KURT
Kürşad ASAN
Gürsel KANSUN
author_sort Oktay KILIÇ
collection DOAJ
description In the north of Pasinler (Erzurum), Upper Miocene-Pliocene volcanic rocks crop out. These volcanites are composed of basaltic andesite, andesite, dacite, rhyolite lavas and rhyolitic pyroclastics. The rocks show porphyritic, microlitic porphyritic, hyalo-microlitic porphyritic, vitrophyric, glomeroporphyritic, pilotaxitic and hyalopilitic textures. The investigated volcanites contain plagioclase (An29-80), olivine (Fo65-82), clinopyroxene (augite), orthopyroxene (enstatite), amphibole (Mg#: 0.57-0.71), biotite (phlogopite: 0.44-0.47, annite: 0.33-0.37), sanidine, quartz and opaque mineral (titano-magnetite and ilmenite). The volcanic rocks are calc-alkaline in character and have medium to high-K contents. Major oxide and trace element variations point out open-system magmatic differentiation in the evolution of rocks. Geochemical data indicate an important role of fractionation of phenocryst phases in the rocks during differentiation process. However, it is considered that assimilation±magma mixing might have accompanied to the process. High LILE (K, Rb, Ba, Th) and relatively low HFSE (Nb, Ta, Hf, Zr) contents of the rocks indicate that these rocks derived from parental magmas carrying subduction signature.
first_indexed 2024-04-10T10:56:00Z
format Article
id doaj.art-0c142477bccf47479f63d18e5538b5c9
institution Directory Open Access Journal
issn 1300-7009
2147-5881
language English
last_indexed 2024-04-10T10:56:00Z
publishDate 2009-02-01
publisher Pamukkale University
record_format Article
series Pamukkale University Journal of Engineering Sciences
spelling doaj.art-0c142477bccf47479f63d18e5538b5c92023-02-15T16:19:56ZengPamukkale UniversityPamukkale University Journal of Engineering Sciences1300-70092147-58812009-02-011522532625000082890Mineral Chemistry and Geochemistry of Volcanic Rocks in The North of Pasinler (Erzurum)Oktay KILIÇHüseyin KURTKürşad ASANGürsel KANSUNIn the north of Pasinler (Erzurum), Upper Miocene-Pliocene volcanic rocks crop out. These volcanites are composed of basaltic andesite, andesite, dacite, rhyolite lavas and rhyolitic pyroclastics. The rocks show porphyritic, microlitic porphyritic, hyalo-microlitic porphyritic, vitrophyric, glomeroporphyritic, pilotaxitic and hyalopilitic textures. The investigated volcanites contain plagioclase (An29-80), olivine (Fo65-82), clinopyroxene (augite), orthopyroxene (enstatite), amphibole (Mg#: 0.57-0.71), biotite (phlogopite: 0.44-0.47, annite: 0.33-0.37), sanidine, quartz and opaque mineral (titano-magnetite and ilmenite). The volcanic rocks are calc-alkaline in character and have medium to high-K contents. Major oxide and trace element variations point out open-system magmatic differentiation in the evolution of rocks. Geochemical data indicate an important role of fractionation of phenocryst phases in the rocks during differentiation process. However, it is considered that assimilation±magma mixing might have accompanied to the process. High LILE (K, Rb, Ba, Th) and relatively low HFSE (Nb, Ta, Hf, Zr) contents of the rocks indicate that these rocks derived from parental magmas carrying subduction signature.http://dergipark.ulakbim.gov.tr/pajes/article/view/5000088821Pasinler, Mineral kimyası, Jeokimya, Kalkalkali volkanitler.
spellingShingle Oktay KILIÇ
Hüseyin KURT
Kürşad ASAN
Gürsel KANSUN
Mineral Chemistry and Geochemistry of Volcanic Rocks in The North of Pasinler (Erzurum)
Pamukkale University Journal of Engineering Sciences
Pasinler, Mineral kimyası, Jeokimya, Kalkalkali volkanitler.
title Mineral Chemistry and Geochemistry of Volcanic Rocks in The North of Pasinler (Erzurum)
title_full Mineral Chemistry and Geochemistry of Volcanic Rocks in The North of Pasinler (Erzurum)
title_fullStr Mineral Chemistry and Geochemistry of Volcanic Rocks in The North of Pasinler (Erzurum)
title_full_unstemmed Mineral Chemistry and Geochemistry of Volcanic Rocks in The North of Pasinler (Erzurum)
title_short Mineral Chemistry and Geochemistry of Volcanic Rocks in The North of Pasinler (Erzurum)
title_sort mineral chemistry and geochemistry of volcanic rocks in the north of pasinler erzurum
topic Pasinler, Mineral kimyası, Jeokimya, Kalkalkali volkanitler.
url http://dergipark.ulakbim.gov.tr/pajes/article/view/5000088821
work_keys_str_mv AT oktaykilic mineralchemistryandgeochemistryofvolcanicrocksinthenorthofpasinlererzurum
AT huseyinkurt mineralchemistryandgeochemistryofvolcanicrocksinthenorthofpasinlererzurum
AT kursadasan mineralchemistryandgeochemistryofvolcanicrocksinthenorthofpasinlererzurum
AT gurselkansun mineralchemistryandgeochemistryofvolcanicrocksinthenorthofpasinlererzurum