The result shows an increasing trend of (C 29 + C 30 ) dishopanes/(C 29 + C 30 ) hopanes values with the increasing of C 24 Tet/C 26 TT values, indicating the formation of diahopane compounds likely related to a reducing and evaporative environment.
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Effect of Depositional Environment on the Occurrence of 17α(H)-Diahopanes in Triassic Lacustrine Sediments from the Ordos Basin, NW China.
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