Mineralogy and geochemistry of granitoids from Kinnaur region, Himachal Higher Himalaya, India: Implication on the nature of felsic magmatism in the collision tectonics

作者：Singh Brajesh; Kumar Santosh^*; Ban Masao; Nakashima Kazuo

来源：Journal of Earth System Science, 2016, 125(7): 1329-1352.

DOI：10.1007/s12040-016-0748-0

• Mineralogy
• geochemistry
• petrogenesis
• granitoids
• Himachal Higher Himalaya

Felsic magmatism in the southern part of Himachal Higher Himalaya is constituted by Neoproterozoic granite gneiss (GGn), Early Palaeozoic granitoids (EPG) and Tertiary tourmaline-bearing leucogranite (TLg). Magnetic susceptibility values (<3x10(-3) SI), molar Al2O3/(CaO+Na2O+K2O) (>= 1.1), mineral assemblage (bt-ms-pl-kf-qtz +/- tur +/- ap), and the presence of normative corundum relate these granitoids to peraluminous S-type, ilmenite series (reduced type) granites formed in a syncollisional tectonic setting. Plagioclase from GGn (An(10)-An(31)) and EPG (An(15)-An(33)) represents oligoclase to andesine and TLg (An(2)-An(15)) represents albite to oligoclase, whereas compositional ranges of K-feldspar are moreor- less similar (Or(88) to Or(95) in GGn, Or(86) to Or(97) in EPG and Or(87) to Or(94) in TLg). Biotites in GGn (Mg/Mg+Fe-t = 0.34-0.45), EPG (Mg/Mg+Fe-t = 0.27-0.47), and TLg (Mg/Mg+Fe-t = 0.25-0.30) are ferribiotites enriched in siderophyllite, which stabilised between FMQ and HM buffers and are characterised by dominant 3Fe reversible arrow 2Al, 3Mg reversible arrow 2Al substitutions typical of peraluminous (S-type), reducing felsic melts. Muscovite in GGn (Mg/Mg+Fe-t = 0.58-0.66), EPG (Mg/Mg+Fe-t = 0.31-0.59), and TLg (Mg/Mg+Fe-t = 0.29-0.42) represent celadonite and paragonite solid solutions, and the tourmaline from EPG and TLg belongs to the schorl-elbaite series, which are characteristics of peraluminous, Li-poor, biotite-tourmaline granites. Geochemical features reveal that the GGn and EPG precursor melts were most likely derived from melting of biotite-rich metapelite and metagraywacke sources, whereas TLg melt appears to have formed from biotite-muscovite rich metapelite and metagraywacke sources. Major and trace elements modelling suggest that the GGn, EPG and TLg parental melts have experienced low degrees (similar to 13, similar to 17 and similar to 13%, respectively) of kf-pl-bt fractionation, respectively, subsequent to partial melting. The GGn and EPG melts are the results of a pre-Himalayan, syn-collisional Pan-African felsic magmatic event, whereas the TLg is a magmatic product of Himalayan collision tectonics.

• 出版日期2016-10