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- W2368091475 abstract "Crustal refusion and intrusion of 揝?type granites possibly occur due to large scale crustal detachment and reversed thrust-contraction. As a result cold crust turned to a thermal one. At centers of deep-fusion granites or refusing and rising old metamorphous complex, thermal uplift structure was formed. The vertical main-strain leads to extension and thinning of the upper crust. The extensional structures include shallow and deep ones. Evidence showing the structures was obtained in 1999 in the Zhifang area of East Junggar near Balikun, covering 220 square kilometers. The core of the structure is composed of Erhuzishan super-unit of refused intrusive granites of early Carboniferous age. The single-Zr Pb/Pb age of granodiorites is 325±48 Ma, and the Rb/Sr age of monzonitic granites is 326±86 Ma. The capping rocks and country rocks are quartz diorites and monzonitic mylonites with zircon 207Pb/206Pb age of 830 Ma. The main detachment surface sits on top of the mylonites, separating from upper metamorphic rocks of the middle Proterozoic. There are two secondary detachment faults, with splitting age of 273 Ma on both southern and northern sides. Subsequent tectonic movement causes the overlapping of metamorphic rocks over Upper Carboniferous and Jurassic rocks." @default.
- W2368091475 created "2016-06-24" @default.
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- W2368091475 date "2002-01-01" @default.
- W2368091475 modified "2023-09-23" @default.
- W2368091475 title "DETERMINATION OF THERMAL-UPLIFT EXTENSIONAL STRUCTURES ALONG BAOERQIANGJI,EAST JUNGGAR" @default.
- W2368091475 hasPublicationYear "2002" @default.
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