Petrology and geochemistry of mantle peridotites from the Kalaymyo and Myitkyina ophiolites (Myanmar): Implications for tectonic settings

Lithos ◽  
2016 ◽  
Vol 264 ◽  
pp. 495-508 ◽  
Author(s):  
Chuan-Zhou Liu ◽  
Chang Zhang ◽  
Yang Xu ◽  
Jian-Gang Wang ◽  
Yi Chen ◽  
...  
Minerals ◽  
2019 ◽  
Vol 9 (6) ◽  
pp. 339 ◽  
Author(s):  
Yang Xu ◽  
Chuan-Zhou Liu

Compositions of highly siderophile elements (HSEs) in forearc mantle have been little studied and effects of slab dehydration on their abundances in forearc mantle remains unclear. This study reports two different kinds of HSE patterns for peridotites from a New Caledonia forearc ophiolite. The Group-I samples show relatively flat patterns of Ir-group-platinum-group elements (IPGEs) and enrichment of Pt over Pd. Such patterns imply that interstitial sulfides were significantly removed through melt extraction, whereas sulfides enclosed within silicates were mostly unaffected. Meanwhile, Pt-Fe alloys were generated, resulting in suprachondritic Pt/Pd ratios. In contrast, the Group-II samples display convex HSE patterns and are depleted in all HSEs except for Ru, yielding strongly positive Ru anomalies. This indicates that both enclosed and interstitial sulfides were substantially consumed, whereas chromite was generated to stabilize Ru. Compared to abyssal peridotites, subduction-related peridotites commonly have stronger fractionation in the HSEs. Therefore, the HSE data of mantle peridotites are potentially able to discriminate the tectonic settings of ophiolites.


2017 ◽  
Vol 9 (1) ◽  
Author(s):  
Sonia Alejandra Torres-Sánchez ◽  
Carita Augustsson ◽  
Uwe Jenchen ◽  
J. Rafael Barboza-Gudiño ◽  
Eduardo Alemán Gallardo ◽  
...  

AbstractThe Granjeno Schist is a meta-volcanosedimentary upper Paleozoic complex in northeastern Mexico. We suggest different tectonic settings for metamorphism of its serpentinite and talc-bearing rocks based on petrographic and geochemical compositions. According to the REE ratios (La


2021 ◽  
Author(s):  
Tamás Sági ◽  
Szabolcs Harangi ◽  
Theodoros Ntaflos

Besides mantle peridotites primary basaltic melts are the best tool to investigate upper mantle petrology and geochemistry. However, de facto primitive melts are hard to found, as basaltic melts usually go through a fractionation process during their ascent towards the surface. Most primary melt calculators are based on the major or trace element compositions of olivine-phyric ocean island basalts and peridotites and are less accurate if clinopyroxene fractionation occurred. In this chapter a new fractionation modeling method of alkaline basalts will be introduced, which has been published earlier only in Hungarian. Olivine ± clinopyroxene fractionation of four basaltic volcanoes have been modeled from different Miocene-Quaternary volcanic fields from the Carpathian-Pannonian Region (Stiavnica (Selmec) VF, Novohrad-Gemer (Nógrád-Gömör) VF, Perşani Mts. (Persányi Mts.) VF and from the Lucaret-Sanoviţa (Lukácskő-Sziklás) volcano.


2013 ◽  
Vol 32 (5) ◽  
pp. 57-66 ◽  
Author(s):  
Lei XU ◽  
Sanzhong LI ◽  
Xin LIU ◽  
Yanhui SUO ◽  
Qi WU ◽  
...  

2017 ◽  
Author(s):  
Paul T. Robinson ◽  
◽  
Jingsui Yang ◽  
Jianwei Li ◽  
Zhang Duan ◽  
...  

Sign in / Sign up

Export Citation Format

Share Document