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Publikováno v:
Journal of Physics: Conference Series. 1363:012034
The Belimbing Field S layer is a layer of the Upper Talangakar Formation (TRM) with a transition precipitation environment deposited in the syn-rift phase with the upper Oligocene lifetime up to the lower Miocene productively producing oil. This is a
Publikováno v:
Journal of Physics: Conference Series; 2019, Vol. 1363 Issue 1, p1-1, 1p