Detailed geochemistry and K-Ar geochronology of the metamorphic sole rocks and their mafic dykes from the Mersin ophiolite, Southern Turkey

Ömer Faruk ÇELİK (Kocaeli Üniversitesi, Mühendislik Fakültesi, Jeoloji Mühendisliği Bölümü, Kocaeli, Türkiye)
Turkish Journal of Earth Sciences
3 0
Yıl: 2008 Cilt: 17 Sayı: 4 Sayfa Aralığı: 685 - 708 Metin Dili: Türkçe İndeks Tarihi: 29-07-2022

Detailed geochemistry and K-Ar geochronology of the metamorphic sole rocks and their mafic dykes from the Mersin ophiolite, Southern Turkey

Öz:
Mersin ofiyolitine ait manto peridotitlerinin tabanında yer alan metamorfik taban kayaçları amfibolitlerden ve metasedimanter litolojilerden meydana gelir. Metamorfik taban kayaçları içerisindeki mineral birliktelikleri, bu kayaçların amfibolit ve yeşilşist fasiyesi toplulukları olduğunu gösterir. Mineral topluluklarına ve minerallerin kimyasal bileşimlerine dayalı jeotermobarometre çalışmaları, metamorfizma esnasındaki metamorfik sıcaklığın 522 ± 15 °C ve basıncın 5 kb’dan az olduğuna işaret eder. Metamorfik taban kayaçlarından amfibolitlerin ana, iz ve nadir toprak elementleri bileşimlerine dayalı jeokimyası, bu kayaçların Yitim Zonu Üstü (SSZ) tipi ofiyolitlerin jeokimyasal özelliklerine sahip olduklarını gösterir. Amfibolitlerin Th/Nb oranları, ortalama değer Okyanus Ortası Sırtı Bazaltlarından (MORB) ve Okyanus Adası Bazaltlarından (OIB) yüksektir. Bu durum muhtemel olarak bu kayaçların yitim bileşeninin etkisiyle zenginleşen manto kaynağının değişmesi sonucu oluştuklarını gösterir. Amfibolitlerin Adayayı Toleyitleri (IAT), OIB ve MORB benzeri jeokimyası, bu kayaçların köken kayaçlarının Yitim Zonu Üstü ortam koşulları içerisinde oluştuklarını ve Batı Pasifikteki Mariana Trough ve Güney Atlantik Okyanusunda, Güney Sandwich yay-basen sistemlerine benzerlik sunduklarını gösterir. İzole dolerit daykları, metamorfik taban kayaçlarına ve ofiyolitik üniteye farklı yapısal seviyelerde sokulum yaparlar. Metamorfik taban kayaçlarını kesen dolerit daykları Adayayı Toleyitleri benzeri jeokimya gösterirler. Bu kayaçlar LIL elementler bakımından zenginleşmişler buna karşın HFS elementler bakımından tüketilmişlerdir. Dolerit dayklarının göreceli düz nadir toprak elementleri gidişleri de bu kayaçların yitim ile ilişkili kökenlerini teyit eder. Metamorfik taban kayaçlarının SSZ özelliklerini göstermeleri ve metamorfik olmayan Adayayı Toleyitleri benzeri dolerit daykları tarafından kesildikleri için Neotetis Okyanusunda dayklar ve metamorfik taban kayaçlarının gelişimini açıklamak için çift yitim sonucuna varılır.
Anahtar Kelime:

Konular: Jeoloji

Mersin ofiyolitinden metamorfik taban kayaçları ve mafik daykların ayrıntılı jeokimyası ve K-Ar jeokronolojisi, Güney Türkiye

Öz:
The metamorphic sole rocks at the base of mantle peridotites from the Mersin ophiolite consist of amphibolites and metasedimentary lithologies. Mineral parageneses in the metamorphic sole rocks exhibit amphibolite and greenschist facies assemblages. Geothermobarometric studies based on mineral assemblages and chemical compositions of minerals indicate that average metamorphic temperature during the metamorphism was 522 ± 15 °C and the pressure was less than 5 kb. Amphibolites from the metamorphic sole rocks exhibit geochemical characteristics of a supra-subduction zone (SSZ) type ophiolite, based on their major, trace and rare earth element (REE) compositions. The Th/Nb ratios of the amphibolites are higher than the average mid-ocean ridge basalt (MORB) and ocean island basalt (OIB) values. This may suggest that they were probably derived from an enriched mantle source modified by the addition of subduction component. Island arc tholeiite (IAT), OIB and MORB-like geochemistry of the amphibolites suggest that protoliths of these rocks were formed in a SSZ environment similar to the South Sandwich arc-basin system from South Atlantic ocean and the Mariana Trough from the Western Pacific. Isolated dolerite dykes intrude both the metamorphic sole rocks and the ophiolitic units at different structural levels. Dolerite dykes cutting the metamorphic sole rocks exhibit IAT-like geochemistry. They are enriched in large-ion-lithophile elements (LILE), depleted in high-field-strength elements (HFSE) and have relatively flat REE patterns, which also confirm their subduction-related origin. Double subduction is inferred here to explain the generation of the metamorphic sole rocks and dykes in the Neotethyan ocean, since the metamorphic sole rocks exhibit SSZ characteristics and were intruded by unmetamorphosed IAT-like dolerite dykes.
Anahtar Kelime:

Konular: Jeoloji
Belge Türü: Makale Makale Türü: Araştırma Makalesi Erişim Türü: Erişime Açık
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APA ÇELİK Ö (2008). Detailed geochemistry and K-Ar geochronology of the metamorphic sole rocks and their mafic dykes from the Mersin ophiolite, Southern Turkey. , 685 - 708.
Chicago ÇELİK ÖMER FARUK Detailed geochemistry and K-Ar geochronology of the metamorphic sole rocks and their mafic dykes from the Mersin ophiolite, Southern Turkey. (2008): 685 - 708.
MLA ÇELİK ÖMER FARUK Detailed geochemistry and K-Ar geochronology of the metamorphic sole rocks and their mafic dykes from the Mersin ophiolite, Southern Turkey. , 2008, ss.685 - 708.
AMA ÇELİK Ö Detailed geochemistry and K-Ar geochronology of the metamorphic sole rocks and their mafic dykes from the Mersin ophiolite, Southern Turkey. . 2008; 685 - 708.
Vancouver ÇELİK Ö Detailed geochemistry and K-Ar geochronology of the metamorphic sole rocks and their mafic dykes from the Mersin ophiolite, Southern Turkey. . 2008; 685 - 708.
IEEE ÇELİK Ö "Detailed geochemistry and K-Ar geochronology of the metamorphic sole rocks and their mafic dykes from the Mersin ophiolite, Southern Turkey." , ss.685 - 708, 2008.
ISNAD ÇELİK, ÖMER FARUK. "Detailed geochemistry and K-Ar geochronology of the metamorphic sole rocks and their mafic dykes from the Mersin ophiolite, Southern Turkey". (2008), 685-708.
APA ÇELİK Ö (2008). Detailed geochemistry and K-Ar geochronology of the metamorphic sole rocks and their mafic dykes from the Mersin ophiolite, Southern Turkey. Turkish Journal of Earth Sciences, 17(4), 685 - 708.
Chicago ÇELİK ÖMER FARUK Detailed geochemistry and K-Ar geochronology of the metamorphic sole rocks and their mafic dykes from the Mersin ophiolite, Southern Turkey. Turkish Journal of Earth Sciences 17, no.4 (2008): 685 - 708.
MLA ÇELİK ÖMER FARUK Detailed geochemistry and K-Ar geochronology of the metamorphic sole rocks and their mafic dykes from the Mersin ophiolite, Southern Turkey. Turkish Journal of Earth Sciences, vol.17, no.4, 2008, ss.685 - 708.
AMA ÇELİK Ö Detailed geochemistry and K-Ar geochronology of the metamorphic sole rocks and their mafic dykes from the Mersin ophiolite, Southern Turkey. Turkish Journal of Earth Sciences. 2008; 17(4): 685 - 708.
Vancouver ÇELİK Ö Detailed geochemistry and K-Ar geochronology of the metamorphic sole rocks and their mafic dykes from the Mersin ophiolite, Southern Turkey. Turkish Journal of Earth Sciences. 2008; 17(4): 685 - 708.
IEEE ÇELİK Ö "Detailed geochemistry and K-Ar geochronology of the metamorphic sole rocks and their mafic dykes from the Mersin ophiolite, Southern Turkey." Turkish Journal of Earth Sciences, 17, ss.685 - 708, 2008.
ISNAD ÇELİK, ÖMER FARUK. "Detailed geochemistry and K-Ar geochronology of the metamorphic sole rocks and their mafic dykes from the Mersin ophiolite, Southern Turkey". Turkish Journal of Earth Sciences 17/4 (2008), 685-708.
Sayfa Oluşturulma Tarihi
09-05-2024 16:5

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