Source-to-sink of Late carboniferous Ordos Basin: Constraints on crustal accretion margins converting to orogenic belts bounding the North China Block

The Upper Carboniferous Benxi Formation of the Ordos Basin is the lowest strata overlying Middle Ordovician above the major ca. 150-Myr sedimentary gap that characterizes the entire North China Block (NCB). We apply an integrated analysis of stratigraphy, petrography, and U–Pb dates and Hf isotopes...

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Detalhes bibliográficos
Main Authors: Anqing Chen, Hao Zou, James G. Ogg, Shuai Yang, Mingcai Hou, Xiuwei Jiang, Shenglin Xu, Xiaoxing Zhang
Formato: Artigo
Idioma:Inglês
Publicado em: Elsevier 2020-11-01
Colecção:Geoscience Frontiers
Assuntos:
Benxi formation
Detrital zircons
Central asian orogen belt
Tectonics
Paleogeography
Moscovian and kasimovian
Acesso em linha:http://www.sciencedirect.com/science/article/pii/S1674987120301274
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