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The oldest erosion surface, SE1, formed across Upper Oligocene Lower Miocene synorogenic deposits; while surface SE2 was contemporaneous with the Middle Miocene alluvial systems, ending with an uplift stage in the Astaracian.
This evolutionary model of the structures present to us is a distinct and intuitive top-popup fold with low amplitude and relatively low-density fractures in the top, has only experienced pre-folding stage and strong folding stage, and has not yet been developed to vertical uplift stage.
Some hydrocarbon was expelled at the early uplift stage (27 23 Ma).
This age is consistent with the initial uplift stage of the OBR at 12 9 Ma (Nakajima et al. 2006).
To consider only the rupture of rock caused by the change of formation, pressure in the uplift stage does not enable an accurate assessment of the sealing ability.
The strata in Es 4 x were thought to have been buried relatively deeply during the uplift stage; thus, meteoric fresh water had a weak effect on reservoir reconstruction.
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The AHe and the ZHe ages younger than 15 Ma overlap with the three known uplift stages (Fig. 4a).
The first phase was from the late Dongying depositional period of the Oligocene to the early uplift stages of the late Paleogene.
Even though some of the He ages might reflect a cooling from the temperatures at which He ages partially reset, it is likely that the cooling was derived from one of the three uplift stages.
On the basis of sedimentary facies analyses, three uplift stages were identified in the OBR as (1) surface uplift and regional unconformity (12 9 Ma), (2) differential uplift and compression (6.5 3 Ma), and (3) uplift and intense compression (after ~3 Ma) (Nakajima et al. 2006; Nakajima 2012, 2013).
In addition, uplift stages in the Dewa Hills and the Asahi Mountains on the back-arc side were constrained by analyzing sedimentary facies in the adjacent Shinjo basin, suggesting that the oldest uplift phase of the Asahi Mountains occurred at ~5 Ma and then the Dewa Hills began to uplift over the Pliocene (Moriya et al. 2008).
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