Geochemistry and geochronology of Mississippian volcanic rocks from SW Mongolia: Implications for terrane subdivision and magmatic arc activity in the Trans-Altai Zone
Abstract
Baaran and Baytag "terranes" form important part of the Trans-Altai Zone of the Central Asian Orogenic Belt in the SW Mongolia. The Trans-Altai Zone represents an oceanic domain built by Ordovician to Devonian ophiolites covered by Devonian-Carboniferous oceanic sediments.
This oceanic assemblage was intruded by a spectrum of Carboniferous volcanic rocks ranging from basalts to rhyolites (325.6 +/- 1.4 Ma to 351.0 +/- 5.9 Ma; LA-ICP-MS U-Pb dating on zircon) that display similar whole-rock trace-element and Sr-Nd isotopic signatures regardless their silica contents and the "terrane" they belong to. They are normal-K calc-alkaline rocks whose NMORB-normalized multielement patterns show an arc-like enrichment in LILE (Large Ion Lithophile Elements) and deep negative TNT (Ta, Nb, Ti) anomalies.
Based on the relatively high Nb/Yb and Th/Yb ratios, the arc was probably formed on immature continental rather than typical oceanic crust. Low (Sr-87/Sr-86)1 (0.7043-0.7047), high epsilon(350)(Nd) (+5.2 to = +5.8) and the observed in-situ Hf isotopic variation in dated zircons (epsilon(t)(Hf) = +7.4 to +13) are all attributed to a partial melting of primitive and youthful (Neoproterozoic-Ordovician) arc-type lower continental crust (metamorphosed intermediate-acid igneous rocks and/or arc-derived greywackes), augmented with, and most likely facilitated by, contemporaneous arc-related basaltic intrusions.
A distinct possibility remains the previously formulated model assuming that the Carboniferous magmatism in Gobi-Altai and Trans-Altai zones sampled the juvenile Neoproterozoic to Cambrian arc crust relaminated under the Ordovician-Devonian oceanic crust. In any case, the studied arc association, together with lithological sequence of ophiolites, can be closely correlated with the Dulate arc in eastern Junggar.
It is proposed that the two arc sequences form a single belt, c. 500 km long, that represents one of the main known arc structures in the Central Asian Orogenic Belt.