Permian age of orogenic thickening and crustal melting in the Garm Block, South Tien Shan, Tajikistan

• Published in: Journal of Asian earth sciences 2015-12, Vol.113, p.711-727
• Main Authors: Konopelko, D., Klemd, R., Mamadjanov, Y., Hegner, E., Knorsch, M., Fidaev, D., Kern, M., Sergeev, S.
• Format: Article
• Language: English
• Subjects: Garm Block; Nd isotopes; Permian metamorphism; South Tien Shan (Tianshan); Tajikistan; Zircon ages
• ISSN: 1367-9120; 1878-5786
• DOI: 10.1016/j.jseaes.2015.09.004

[Display omitted] •First Early Permian regional metamorphism in CAOB established in Garm Block.•A 290Ma age of crosscutting granite is identical to the age of metamorphism.•Ediacarian maximum depositional age established for metasedimentary schists.•Nd data indicate major input of Paleoproterozoic crustal component. In this paper we present new data for the metamorphic Garm Block (150×40km) that was traditionally shown on regional maps as fragment of a Precambrian basement. The Garm Block comprises migmatized gneisses and schists for some of which peak metamorphic conditions (600–660°C at 7–9kbar) characteristic for medium P/T series metamorphic belts were determined. U–Pb ages of overgrown rims of zircon grains and newly grown magmatic zircon grains from four migmatitic samples indicate that melting occurred during peak metamorphic conditions between 299 and 290Ma. Thus the Garm Block is the first Early Permian regional metamorphic terrane established in the southern part of the Central Asian Orogenic Belt. A crosscutting granite intrusion yields a concordia age of 290Ma identical to the age of metamorphism and similar to ages of post-collisional intrusions elsewhere in the Tien Shan. Detrital zircon grains from the Garm samples yield an age spectrum with major peaks at 700–550Ma and 1150–700Ma, and smaller ones at ca. 2.7–2.4Ga and 3.5–3.3Ga. The youngest grains define an Ediacarian maximum depositional age of the sedimentary protoliths. The presence of Grenvillian ages of 1150–800Ma, which are characteristic for the Tarim Craton, and the lack of ca. 1.6–1.2Ga ages, characteristic for the Northern Tien Shan, suggest an origin of the Precambrian zircon grains from southern continental blocks similar to the Tarim Craton. Six granitoid samples yield negative εNd values of −10.6 to −3.7 consistent with the reworking of crustal material with 1.8–1.1Ga average crustal residence times and the formation of the South Tien Shan belt on a continental basement with Paleoproterozoic or older crust. The Garm Block formed as a consequence of lithospheric thickening during the Late Carboniferous collision of two continental blocks that created the South Tien Shan fold belt. Lateral crustal melt flow coupled with extension may have resulted in exhumation of the Permian metamorphic rocks.