Details

Autor(en) / Beteiligte

• Gong, Junfeng
• Ji, Jianqing
• Han, Baofu
• Chen, Jianjun
• Sun, Dongxia
• Li, Baolong
• Zhou, Jing
• Tu, Jiyao
• Zhong, Dalai

Titel

Early subduction-exhumation and late channel flow of the Greater Himalayan Sequence: implications from the Yadong section in the eastern Himalaya

Ist Teil von

• International geology review, 2012-07, Vol.54 (10), p.1184-1202

Ort / Verlag

Philadelphia: Taylor & Francis

Erscheinungsjahr

2012

Link zum Volltext

Quelle

Taylor & Francis

Beschreibungen/Notizen

• Based on metamorphic studies of the Yadong high-pressure (HP) granulite and multiple thermochronological investigations of granitoids from both upper and lower parts, the Yadong section in the eastern Himalaya constrains the Cenozoic tectonic evolution of the Greater Himalayan Sequence (GHS). The Yadong HP granulite, located at the top of the GHS, underwent a peak-stage HP granulite facies metamorphism and two stages of retrograde metamorphism. Granulite and hornblende facies retrograde metamorphism took place at 48.5 and 31.8 Ma, respectively, marking the time of exhumation of the subducted Indian slab to lower and middle crustal levels. Subsequently, an average young zircon U-Pb age obtained from the Yadong HP granulite indicated that this unit was captured by its surroundings in a partially molten condition at 16.9 Ma. In addition, three granitoids from both the lower and the upper parts of the GHS yielded biotite 40 Ar/ 39 Ar ages of 11.0, 11.3, and 11.5 million years. These consistent ages suggest that the GHS along the Yadong section was laterally extruded and synchronously cooled to ∼300°C at ∼11.3 Ma. Furthermore, the granitic gneisses yield apatite fission track ages of ∼7 million years, documenting the cooling of the GHS to ∼110°C. A two-stage model describes the Cenozoic tectonic evolution of the GHS: (1) the Indian slab had subducted under Tibet before ∼55 Ma, and was exhumed to the lower crust (50-40 km) at 48.5 Ma, and to the middle crust (22-15 km) at 31.8 Ma; and (2) the partial melting occurred at middle crustal levels during the period 31.8 to 16.9 Ma, causing channel flow. In the late stage, the GHS was laterally extruded by ductile mid-crustal flow during the period 16.9 to ∼7 Ma, characterized by a fast cooling rate of ∼2 mm per year.