| dc.creator |
Tükel, Fatma Şişman |
|
| dc.creator |
CARAN, Şemsettin |
|
| dc.creator |
Yesiltas, Mehmet |
|
| dc.creator |
AYSAL, NAMIK |
|
| dc.creator |
Yagcioglu, Kıymet Deniz |
|
| dc.creator |
YILMAZ, İSAK |
|
| dc.creator |
ÖZBEY, ZEYNEP |
|
| dc.date |
2024-11-01T00:00:00Z |
|
| dc.date.accessioned |
2025-02-25T10:17:50Z |
|
| dc.date.available |
2025-02-25T10:17:50Z |
|
| dc.identifier |
1a04b480-515e-475d-8f8c-5f790ad43d66 |
|
| dc.identifier |
10.1016/j.chemer.2024.126126 |
|
| dc.identifier |
https://avesis.sdu.edu.tr/publication/details/1a04b480-515e-475d-8f8c-5f790ad43d66/oai |
|
| dc.identifier.uri |
http://acikerisim.sdu.edu.tr/xmlui/handle/123456789/98929 |
|
| dc.description |
The Menderes massif is a large metamorphic crystalline complex located in western Turkey. The massif consists of late Neoproterozoic basement (core) rocks and Palaeozoic - Cenozoic cover units that have undergone by high- and low-grade polyphase metamorphisms. Palaeozoic to Mesozoic cover units cropped out in the NE edge of the massif (east of Sivaslı) are overlaid tectonically by upper Cretaceous meta-ophiolitic rocks. The meta-ophiolitic unit comprises blocks mainly of metabasalt, metagabbro, metadiorite and metaultramafite within an intensively sheared serpentinite matrix. It also includes blocks of epidote-actinolite-schist and tremolite-actinolite-schist, which originated from basic rocks, as well as chlorite schist blocks, which originated from ultramafic rocks. Sodic-calcic amphiboles recorded in the samples of metabasalt block taken from the marble-metabasalt block boundary, at the tectonic contact where the meta-ophiolitic rocks overlap the underlying marble sequence. Sodic-calcic amphiboles were classified into winchite and ferri-winchite with relatively homogeneous TSi (7.35–8.01 a.p.f.u.), and XMg (0.69–0.80) values. P-T conditions were estimated to be around 300–400 °C and 5–6 kb based on the mineral chemical analyses of the sodic-calcic amphiboles. According to these values, the NE edge of the Menderes Massif must have undergone metamorphism under a medium-pressure (MP) greenschist facies. |
|
| dc.language |
eng |
|
| dc.rights |
info:eu-repo/semantics/closedAccess |
|
| dc.title |
Mineral chemistry and P–T conditions of the winchite-bearing metabasic rocks in the NE edge of the Menderes Massif (Western Türkiye) |
|
| dc.type |
info:eu-repo/semantics/article |
|