Sino-Korean Craton (SKC) in eastern China is an important natural laboratory for studying temporal change to the lithosphere because there is the jutaxposition of Ordovician diamondiferous kimberlites, Mesozoic lamprophyre-basalt and Cenozoic tholeiite-alkali basalts in this craton. While diamond ...
First report of Cystostroma (Stromatoporoidea; Ordovician) from Sino-Korean Craton. Geosci. J. 19, 25-31.Oh, J.R., Choh, S.J. & Lee, D.J. 2014: First report of Cystostroma (Stromatoporoidea; Ordovician) from Sino-Korean Craton. Geosciences Journal 19, 25-31....
1998. Nature and evolution of Cenozoic lithospheric mantle beneath Shandong Peninsula, Sino-Korean Craton, eastern China. International Geology Review 40 : 471-499 CrossRef .Zheng J P, O'Reilly S Y, Griffin W L. Nature and evolution of Cenozoic lithospheric mantle beneath Shandong Peninsula, ...
Sino‐Korean CratontrilobitesThe Taebaeksan Basin is located in the mid〆astern part of the southern Korean Peninsula and tectonically belonged to the Sino㎏orean Craton (SKC). It comprises largely the lower Paleozoic Joseon Supergroup and the upper Paleozoic Pyeongan Supergroup which are separated ...
Palaeozoic and Cenozoic lithoprobes and the loss of> 120 km of Archaean lithosphere, Sino-Korean craton, China MA Menzies, W Fan, M Zhang Geological Society, London, Special Publications 76 (1), 71-81 来自 ResearchGate 喜欢 0 阅读量: 335 作者:...
Contrasting Cenozoic Lithospheric Evolution and Architecture in the Western and Eastern Sino-Korean Craton:Constraints from Geochemistry of Basalts and Mantle Xenoliths 来自 万方 喜欢 0 阅读量: 90 作者:J Ma,YG Xu,L Shi,SL Chung 摘要: Cenozoic basalts from both sides of the Daxin'anling-Taihang ...
Sino-Korean CratonBased on published data and original investigations, it has been shown that the combination of widely known Ag, Fe, and Fe-Mn ore deposits, as well as boron and Pb-Zn world-class deposits, is typical for metallogenic zones in the north and northeast of the Sino-Korean ...
Late Ordovician volcanism in Korea constrains the timing for breakup of Sino-Korean Craton from Gondwana. J. Asian Earth Sci. 96, 279-286.Cho, D.-L. et al. Late Ordovician volcanism in Korea constrains the timing for breakup of Sino-Korean Craton from Gondwana. J. Asian Earth Sci. 96,...
Large areas of northern China are underlain by the Sino-Korean Craton, which was stabilized in Early Proterozoic time. However, the eastern part of this craton has been technically active since the late Mesozoic, with the development of large sedimentary basins, high heat flow, extensive ...
Cenozoic basalts from both sides of the Daxin'anling-Taihang gravity lineament that separates the Sino-Korean craton (SKC) into western and eastern parts have been studied. In the western SKC, magmas evolved from xenolith-bearing alkali basalts of Late Eocene-Oligocene age to coexisting alkali and...