Origin and Episodic Emplacement of the Manaslu Intrusive Complex, Central Himalaya
نویسندگان
چکیده
decompression to achieve the same result appear to require extreme The Manaslu granite is the most studied of the dozen or so plutons conditions not permitted by available geological constraints. that make up the High Himalayan leucogranite belt. The inferred relationship of the Manaslu granite with important Himalayan tectonic structures has inspired repeated attempts to determine its crystallization age, but several geochemical controls have hampered these geochronological investigations. These limitations are circumvented by Th–Pb ion microprobe dating of monazite. We have
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دما و فشارسنجی و ژئوشیمی تودههای باردار و عقیم در محور دهج-میدوک با استفاده از شیمی بیوتیت (شمال شهربابک)
Studied rocks are located in Dehaj-Meiduk area north of Shahrbabak.There are eight porphyry intrusive bodies in this region including Meiduk, Parkam, Iejoo, Segino, Narkoh, Ayoub ansar, Sara and Keder that Meiduk, Parkam, Iejoo nad Segino are productive and Narkoh, Ayoub ansar and Sara are barren. The intrusive bodies are composed of quartzdiorite and granodiorite. The intrusive bodies are main...
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, J. Geogr., 106, 156–167.Arita, K., Y. Ohta, C. Akiba, and Y. Maruo (1973),Kathmandu region, in Geology of the Nepal Hima-layas, edited by S. Hashimoto, Y. Ohta, and C. Akiba, pp. 99–145, Saikon, Sapporo, Japan.Arita, K., R. D. Dallmeyer, and A. Takasu (1997),Tectonothermal evolution of the Lesser Himalaya, Nepal: Constraints fromAr/Ar ages from theKathmandu Nappe, ...
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