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摘要:
The Boroujerd pluton (ca 175 Ma) was emplaced in the Sanandaj-Sirjan zone (SSZ) active margin of Central Iran consists of monzogranite, granodiorite, and quartz-diorite. Microstructural studies show a continuum from magmatic to (sub) mylonitic deformations fabric. Intensity of deformation decreases from W-NW to E-SE. The over- all magnetic fabric of the pluton yields steep NW- SE striking foliations and sub-horizontal lineations plunging both to the northwest and south- east. These features imply that during intrusion of the pluton, a NW-SE trending stretching was dominant. This stretching is ascribed to the trans- pressive deformation of the overriding SSZ during northeastward subduction of the Neotethys under the Iranian plate. The NW-SE trending lineations of the Gousheh pluton (ca 35 Ma) suggest that the transpressive regime was ongoing from the Mesozoic to late Eocene.
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篇名 A preliminary study of the anisotropy of magnetic susceptibility (AMS) of Boroujerd granitoids, Sanandaj-Sirjan Zone, West Iran
来源期刊 自然科学期刊(英文) 学科 地球科学
关键词 Gousheh Boroujerd Sanandaj-Sirjan Iran AMS GRANITOID NEOTETHYS
年,卷(期) 2012,(2) 所属期刊栏目
研究方向 页码范围 91-105
页数 15页 分类号 P5
字数 语种
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Gousheh
Boroujerd
Sanandaj-Sirjan
Iran
AMS
GRANITOID
NEOTETHYS
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期刊影响力
自然科学期刊(英文)
月刊
2150-4091
武汉市江夏区汤逊湖北路38号光谷总部空间
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1054
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0
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0
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