Documenting the Partial Melting of Gabbroic Rocks: A Natural Example from the Alvand Plutonic Complex (Northern Sanandaj-Sirjan Zone, West Iran)

被引：0
|
作者：
Lucci, Federico [1 ,2 ,3 ]
Saki, Adel
Miri, Mirmohammad
机构：
[1] Univ Roma Tre, Dipartimento Sci, Rome, Italy
[2] Univ Bari Aldo Moro, Dipartimento Sci Terra & Geoambientali, Bari, Italy
[3] Shahid Chamran Univ Ahvaz, A Saki M Miri Dept Geol, Fac Earth Sci, Ahvaz, Iran
来源：
SELECTED STUDIES IN GEOMORPHOLOGY, SEDIMENTOLOGY, AND GEOCHEMISTRY, CAJG-3 2020 | 2024年
关键词：
Gabbro partial melting; Trondhjemite; Alvand complex; Sanandaj-Sirjan zone; Iran; HORNBLENDE; ORIGIN;
D O I：
10.1007/978-3-031-43744-1_1
中图分类号：
P3 [地球物理学]; P59 [地球化学];
学科分类号：
0708 ; 070902 ;
摘要：
The Alvand Complex in Hamedan area (NW-Iran) represents a key area to document the partial melting of a gabbroic protolith. In this area, where the hornblende-gabbros are in contact with coeval to younger olivine-abbros and pyroxenites, they are characterized by the diffuse presence of trondhjemite leucosomes veins. Equilibrium batch melting modelling indicates trondhjemites as the products of 2-5% degree of partial melting of the hornblende-gabbro. Thermobaric estimates indicate T 720 degrees C and P 3.5 kbar for the anatectic event.
引用
收藏
页码：3 / 6
页数：4
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