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The AAPG/Datapages Combined Publications Database
Journal of Petroleum Geology
Abstract
Journal of Petroleum Geology, vol.
OVERPRESSURE DEVELOPMENT AND HYDROFRACTURING IN THE YINGGEHAI BASIN, SOUTH CHINA SEA
Xie Xinong*+, Li Sitian*, Dong Weiliang** and Zhang Qiming**
Intensely
overpressured compartments are present in the centre of the Yinggehai Basin, South China
Sea. In this part of the basin, a diapiric area can be
distinguished from a non-diapiric area; structures in the former area result from shale
diapirism at depth, and from the movement of hydrothermal
fluids at more shallow levels. In the diapiric zone, the top of the overpressured compartment is relatively shallow (1,500m to
2,500m deep), whereas it is more than 3,200m deep in the non-diapiric area. The top of
the overpressured compartment in the diapiric zone has been
raised to relatively shallow levels due to vertical fluid expulsion
.
Hydrofracturing has
occurred in the Neogene- Quaternary marine sedimentary succession, particularly in
mud-rich intervals such as the Lower Member of the
Pliocene Yinggehai Formation. Hydrofracturing may have allowed the rapid lateral and
vertical migration
of enormous volumes of pore fluids. The
presence of additional steeply-dipping faults in the
diapiric area may have led to vertical
expulsion
of fluids
from overpressured compartments to normally-pressured areas, and caused the top of the
overpressured compartment to be uplifted. Gaseous hydrocarbons are assumed to have
migrated vertically through fractures around diapiric structures from overpressured to
normally-pressured zones. We believe that this mechanism has had a significant effect on
hydrocarbon
transport and
accumulation
in the Yinggehai Basin.
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