The Tectonic Transition from the Paleo-Asian Ocean to the Paleo-Pacific Ocean in Northeastern Eurasia: Constraints from the Early Mesozoic Volcanic-Sedimentary Rocks

Authors: Hong-Yan Wang, Jian-Bo Zhou, Simon A. Wilde

Abstract:

Since the Paleozoic, the tectonic evolution of northeastern Eurasia has been dominated by the Paleo-Asian Ocean and the Paleo-Pacific Ocean tectonic domains. However, the spatiotemporal framework and the timing of the tectonic transition between these two oceanic domains remain enigmatic. To address this issue, this study investigated the petrological, geochronological, and geochemical characters of chlorite schist, andesite and sandstone along the convergent margin (Jilin-Yanji Suture) between the Northeast China terranes and the North China craton in central Jilin Province, China. The results show that the protoliths of chlorite schists and the andesite samples are high-Mg andesites formed in the Early Triassic (249 ± 3 Ma - 246 ± 4 Ma), and their magma source was produced by the metasomatized mantle wedge by subducted slab-derived fluids in a continental island arc setting. The sandstones are immature graywackes with a maximum depositional age of Early Triassic (248 ± 1 Ma), they were formed in a sedimentary basin (most likely an intra-arc basin) intimately associated with one or more continental arcs along the northeastern edge of the North China craton and their sediments were largely derived from coeval magmatic rocks in a juvenile continental arc. Based on the new results and the field investigation, this study suggests that the continental arcs along the northeastern edge of the North China Craton were caused by the southwestward subduction of the Jilin-Heilongjiang Ocean during the early Mesozoic. There is a distinct temporal gap between the closure of the Paleo-Asian Ocean (ca. 260 Ma) and the onset of Paleo-Pacific plate subduction (234–220 Ma), which is essentially coeval with the southwestward subduction of the Jilin-Heilongjiang Ocean between 256 Ma and 239 Ma, meaning the latter is a key link that marks the transition between these two tectonic domains.

Keywords: intra-arc basin, high-Mg andesites, early Mesozoic, Jilin-Heilongjiang Ocean, tectonic transition in northeastern Eurasia