Publication Date:
2019-02-01
Description:
The first offshore gas hydrate production test was conducted within the gas-hydrate-concentrated zone (reservoir)
of the eastern Nankai Trough, which is considered to be a stratigraphic accumulation. However, the
accumulation mechanism for this concentrated zone was not yet well understood. We used core and geophysical
log data sets to determine the subsurface geologic architecture and stratigraphic evolution most likely
responsible for the stratigraphic accumulation of gas hydrate in the eastern Nankai Trough. Seven depositional
sequences were identified based on grain size, bed thickness, sedimentary structure, and stacking patterns. The
sequence boundaries were also identified by terminations of seismic reflection. These sequences were attributed
to a fourth to fifth-order eustatic sea-level changes because the stacking pattern cycle was in phase with
global oxygen isotope curves; the cycle was also identified in the onshore formation during the same period. The
reservoir was interpreted as falling-stage systems tract (FSST) and lowstand systems tract (LST). FSST and LST
consisted mostly of trough-fill channel deposits. The deposits were represented by alternations of very fine- to
fine-grained sand and silt. The reservoir is located in association with the structural wing of the Daini-Atsumi
Knoll. The uplift of the knoll was strongly controlled by tectonic events associated with subduction of the pacific
plate during Pleistocene time. The muddy deposits above the reservoir were interpreted as condensed section.
We identified channel facies pinched out against structural highs, and together, these result in stratigraphic
traps. Consequentially, the gas hydrate trapping system was constrained by sedimentary facies, systems tracts,
and geographic and tectonic setting. Concepts and data generated in this study can be used for gas hydrate
petroleum system analysis such as basin simulation.
Type:
Article
,
PeerReviewed
Format:
text
DOI:
10.1190/INT-2015-0024.1
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