Geological, Structural and Mineralogical Approach to Investigate the Evolution of Low- and very Low-Grade Metamorphic Units from the Intra-Pontide Suture Zone, Central Pontides, Turkey-Reference-Cited by-同舟云学术

Geological, Structural and Mineralogical Approach to Investigate the Evolution of Low- and very Low-Grade Metamorphic Units from the Intra-Pontide Suture Zone, Central Pontides, Turkey

Published:2021-12 Issue:6 Volume:32 Page:1512-1527
ISSN:1674-487X
Container-title:Journal of Earth Science
language:en
Short-container-title:J. Earth Sci.

Author:

Ellero Alessandro^ORCID,Frassi Chiara,Göncüoğlu Mehmet Cemal,Lezzerini Marco,Marroni Michele,Ottria Giuseppe^ORCID,Pandolfi Luca,Sayit Kaan,Tamponi Marco

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

https://link.springer.com/content/pdf/10.1007/s12583-021-1445-8.pdf

Reference82 articles.

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2. Alparslan, G., Dilek, Y., 2018. Seafloor Spreading Structure, Geochronology, and Tectonic Evolution of the Küre Ophiolite, Turkey: A Jurassic Continental Backarc Basin Oceanic Lithosphere in Southern Eurasia. Lithosphere, 10(1): 14–34. https://doi.org/10.1130/l641.1

3. Árkai, P., 1991. Chlorite Crystallinity: An Empirical Approach and Correlation with Illite Crystallinity, Coal Rank and Mineral Facies as Exemplified by Palaeozoic and Mesozoic Rocks of Northeast Hungary. Journal of Metamorphic Geology, 9(6): 723–734. https://doi.org/10.1111/j.1525-1314.1991.tb00561.x

4. Árkai, P., Sassi, F. P., Sassi, R., 1995. Simultaneous Measurements of Chlorite and Illite Crystallinity: A more Reliable Tool for Monitoring Low- to very Low Grade Metamorphisms in Metapelites: A Case Study from the Southern Alps (NE Italy). European Journal of Mineralogy, 7(5): 1115–1128. https://doi.org/10.1127/ejm/7/5/1115

5. Aygül, M., Okay, A. I., Oberhänsli, R., et al., 2016. Pre-Collisional Accretionary Growth of the Southern Laurasian Active Margin, Central Pontides, Turkey. Tectonophysics, 671: 218–234. https://doi.org/10.1016/j.tecto.2016.01.010

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