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SUN Chun-yan, WANG Hong-yu, NIU Bin-hua
China University of Geosciences, Beijing 100083, China
In this paper, studies of method and applicability are
emphasis. With oil and gas geological data、seismic exploration
data and geochemical prospecting data, integrated interpretation
and evaluation research on Xisha trough for the investigation
of gas hydrates are systematical developed. Methods are
also summarized.
In the gas hydrates interpretation research on Xisha ocean
trough, several results are obtained:
(1) Through geomorphologic, depositional and tectonic
conditions analysis, the study area displayed a favorable
gas hydrates investigation prospect. (2) Through structural
interpretation, tectonic features of the research area,
relations between BSR and local structure and structural
effects on gas hydrates formation are made clear. (3) Through
seismic attributes analysis, bottom simulating reflector,
blanking reflector and velocity-amplitude features distribution
regions are pointed out, and bright spots, reversal of poles,
abnormal instantaneous frequency and anomalous AVO attributes
seismic reflection phenomena as well as their relations
are indicated. (4) By geochemistry testing, we found high
gaseous hydrocarbon content regions and summarized rules
of vertical change of hydrocarbon content and their contacts
with depositional environment. (5) The comprehensive identification
of methane carbon isotope and hydrocarbon gas humidity shows
that the most gaseous hydrocarbon in the submarine sediment
in this study region is pyrogenetic with a little part of
biogenetic in addition. Combined with the geology analysis,
we determined that the methane of gas hydrates which may
exist in the sedimentary formation should be pyrogenetic.
(6) The methane gas and gas hydrates model of study area
should be named fault-percolation aggregative model. There
are several gas migration power sources. The fluid courses
are not only faults, but also caused by strata percolation.
That is why non-identity occurs between areas of BSR and
the high methane content in sediments. (7) Finally, through
comprehensive analysis on each aspect, several favorable
marine gas hydrates exploration regions are pointed out
in this paper.
We also found some rules in the geochemistry research
aimed at the gas hydrates prospecting. (1) In the depth
from one meter to four meter below the seafloor, deposition
sample contain abundant information and have highly differentiated
geochemical characteristics. The deep samples are more fit
for geochemical parameters analysis. (2) Measurement by
head space gas sensor is simple and convenient, and is more
fit to test hydrocarbon in field. Acidolysis hydrocarbon
chromatography method is adaptable to in-house procedure.
(3) It’s an effective method to discriminate gaseous hydrocarbon
genesis of submarine sediment through comprehensive identification
of methane carbon isotope and hydrocarbon gas humidity.
And in some means, gaseous hydrocarbon genesis of sediment
can indicate gas hydrates genesis that below these sediment.
(4) Comprehensive analysis on geologic、 geophysical and
geochemical parameters is able to clarity gas hydrates genetic
model and definite favorable exploration target, and can
directly point out the future exploration direction. (5)
Aiming at geochemical prospecting for gas hydrates investigation,
the author has designed a data processing procedure and
a method of quadrant distance reciprocal weighed geology
data interpolation. (6) We conclude that we should introduce
more technologies of geologic evaluation and management
process in oil and gas exploration, make a systematic study
aimed at the importance and effectiveness of every interpretation
and evaluation method, and accomplish a perfect combined
technology system for gas hydrates prospecting study.
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