Middle Ordovician bottom current deposits in the western margin of the North China craton: Evidence from sedimentary and magnetic fabrics
Author:
Affiliation:
1. State Key Laboratory of Biogeology and Environmental Geology School of Earth Sciences China University of Geosciences Wuhan 430074 China
Funder
National Natural Science Foundation of China
Publisher
Wiley
Subject
Stratigraphy,Geology
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1111/sed.12957
Reference110 articles.
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3. Directional petrological characterization of deep‐marine sandstones using grain fabric and permeability anisotropy: methodologies, theory, application and suggestions for integration;Baas J.H.;Earth‐Sci. Rev.,2007
4. Compositional variability of glauconites within the Upper Cretaceous Karai Shale Formation, Cauvery Basin, India: implications for evaluation of stratigraphic condensation;Banerjee S.;Sediment. Geol.,2016
5. Influence of bottom currents on the sedimentary processes at the western tip of the Gulf of Corinth, Greece;Beckers A.;Mar. Geol.,2016
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