Petrology, geochemistry and P–T–t path of lawsonite‐bearing retrograded eclogites in the Changning–Menglian orogenic belt, southeast Tibetan Plateau. (25th December 2018)

• Record Type: Journal Article
• Authors: Wang, Huining; Liu, Fulai; Li, Jing; Sun, Zaibo; Ji, Lei; Tian, Zhonghua; Liu, Lishuang; Santosh, M.
• Is Part Of: Journal of metamorphic geology. Volume 37:Number 4(2019)
• Page Start: 439
• Page End: 478
• Publication Date: 2018-12-25
• Subjects: Changning–Menglian orogenic belt -- geochemistry -- lawsonite‐bearing retrograded eclogite -- Palaeo‐Tethys Ocean -- P–T–t path; Metamorphism (Geology) -- Periodicals; 552.4
• DOI: 10.1111/jmg.12462
• Languages: English
• ISSNs: 0263-4929

Abstract

Abstract: The Changning–Menglian orogenic belt (CMOB) in the southeastern Tibetan Plateau, is considered as the main suture zone marking the closure of the Palaeo‐Tethys Ocean between the Indochina and Sibumasu blocks. Here, we investigate the recently discovered retrograded eclogites from this suture zone in terms of their petrological, geochemical and geochronological features, with the aim of constraining the metamorphic evolution and protolith signature. Two types of metabasites are identified: retrograded eclogites and mafic schists. The igneous precursors of the retrograded eclogites exhibit rare earth element distribution patterns and trace element abundance similar to those of ocean island basalts, and are inferred to have been derived from a basaltic seamount in an intra‐oceanic tectonic setting. In contrast, the mafic schists show geochemical affinity to arc‐related volcanics with the enrichment of Rb, Th and U, and depletion of Nb, Ta, Zr, Hf and Ti, and their protoliths possibly formed at an active continental margin tectonic setting. Retrograded eclogites are characterized by peak metamorphic mineral assemblages of garnet, omphacite, white mica, lawsonite and rutile, and underwent five‐stage metamorphic evolution, including pre‐peak prograde stage (M1 ) at 18–19 kbar and 400–420°C, peak lawsonite‐eclogite facies (M2 ) at 24–26 kbar and 520–530°C, post‐peak epidote–eclogite facies decompression stage (M3 ) at 13–18 kbar and 530–560°C, subsequent amphibolite facies retrogressive stage (M4 ) at 8–10 kbar and 530–600°C, and late greenschist facies cooling stage (M5 ) at 5–8 kbar and 480–490°C. Laser ablation inductively coupled plasma mass spectrometry (LA–ICP–MS) U–Pb spot analyses of zircon show two distinct age groups. The magmatic zircon from both the retrograded eclogite and mafic schist yielded protolith ages of 451 ± 3 Ma, which is consistent with the ages of Early Palaeozoic ophiolitic complexes and ocean island sequences in the CMOB reported in previous studies. In contrast, metamorphic zircon from the retrograded eclogite samples yielded consistent Triassic metamorphic ages of 246 ± 2 and 245 ± 2 Ma, which can be interpreted as the timing of closure of the Palaeo‐Tethys Ocean. The compatible peak metamorphic mineral assemblages, P–T–t paths and metamorphic ages, as well as the similar protolith signatures for the eclogites in the CMOB and Longmu Co–Shuanghu suture (LCSS) suggest that the two belts formed part of a cold oceanic subduction system in the Triassic. The main suture zone of the Palaeo‐Tethyan domain extends at least 1, 500 km in length from the CMOB to the LCSS in the Tibetan Plateau. The identification of lawsonite‐bearing retrograded eclogites in the CMOB provides important insights into the tectonic framework and complex geological evolution of the Palaeo‐Tethys.