Major, trace and platinum-group element geochemistry of the Upper Triassic nonmarine hot shales in the Ordos basin, Central China
•The Upper Triassic Chang 7 hot shales developed under anoxic environment.•Humid paleoclimate was favorable for the deposition of the Chang 7 hot shales.•Tectonics is the major control on the development of the Chang 7 hot shales. The Upper Triassic Chang 7 non-marine hot shales have been proven to...
Saved in:
Published in | Applied geochemistry Vol. 53; pp. 42 - 52 |
---|---|
Main Authors | , , , , , |
Format | Journal Article |
Language | English |
Published |
Elsevier Ltd
01.02.2015
|
Subjects | |
Online Access | Get full text |
Cover
Loading…
Be the first to leave a comment!