Petrology of high‐pressure granulites from the eastern Himalayan syntaxis

The eastern Himalayan syntaxis, situated at the eastern terminus of the Himalayas, is the least‐known segment of the Himalayas. Recent research in this area has revealed that the syntaxis consists of the Gangdise, the Yarlung Zangbo, and the Himalayan units, each of which is bounded by faults. The Himalayan unit, the northernmost exposed part of the Indian plate, mainly contains amphibolite facies rocks, marked by the assemblages staurolite+kyanite+plagioclase+biotite+muscovite±sillimanite and garnet+amphibole+plagioclase, in the south; to the north, low‐ to medium‐pressure granulite grade pelitic gneisses and marbles are present and are characterized by the assemblages garnet+sillimanite+K‐feldspar+plagioclase or antiperthite+biotite+quartz±spinel±cordierite±orthopyroxene in gneisses, and anorthite+diopside±wollastonite and plagioclase+diopside+quartz+phlogopite+calcite in marbles. Within this unit, the Namula thrust system is a series of moderately north‐dipping structures that displaced the granulite facies rocks southwards over the amphibolite facies rocks. High‐pressure granulites occur as relics within these granulite facies rocks and contain garnet–kyanite granulite and garnet clinopyroxenite. The peak assemblage of the garnet–kyanite granulite includes garnet (core part)+kyanite+ternary feldspar+quartz+rutile. Sillimanite+garnet (rim part)+K‐feldspar+ oligoclase+ilmenite+biotite and spinel+albite+biotite or spinel+cordierite±orthopyroxene, which are coronas around sillimanite and garnet, are retrograde products of this peak assemblage. Another peak assemblage includes very‐high‐Ca garnet (CaO 32–34 wt%, Alm 10 ±Grs >80 ) and diopside (CaO 22–24 wt%), scapolite, meionite, quartz, and accessory Al‐bearing titanite (Al 2 O 3 4–4.5 wt%). The diopside has kink bands. Partial or complete breakdown of Ca‐rich garnet during post‐peak metamorphism produced pseudomorphs and coronas consisting of fine‐grained symplectic intergrowths of hedenbergite and anorthite. Thermobarometric estimates in combination with reaction textures, mineral compositions, and recent experimental studies indicate that these peak assemblages were formed at P = c. 1.7–1.8 GPa, T  = c. 890 °C, and the retrograde assemblages experienced near‐isothermal decompression to P =0.5±0.1 GPa, T  =850±50 °C. The whole‐rock compositions indicate that marble and pelite are plausible candidates for the protoliths. These facts suggest the following (1) sedimentary rocks were transported to upper‐mantle depths and equilibrated at those conditions to form these high‐pressure granulites, which were then emplaced into the crust quickly. During the rapid exhumation of these rocks, the earlier high‐pressure assemblages were overprinted by the later low‐ to medium‐pressure assemblages, that is, the high‐pressure granulite belt formed in the syntaxis. (2) The Namula thrust system is an important tectonic boundary in the syntaxis, or even in the Higher Himalaya more generally.