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pro vyhledávání: '"van Loon A.J. [lpar]Tom[rpar]"'
Publikováno v:
Geologos, Vol 25, Iss 1, Pp 15-30 (2019)
The silty top parts of graded turbidites of the Late Ordovician Pingliang Formation, which accumulated along the southern margin of the Ordos Basin (central China), have been reworked by contour currents. The reworking of the turbidites can be proven
Externí odkaz:
https://doaj.org/article/1c7b3426e4654418bebb48ee05abfbfa
