Dalam artikel ini disebut-sebut "chimney cubes", "fault cubes", adakah yg 
tahu detil atau aplikasinya ?

RDP 
=======================
The Geophysical Corner is a regular column in the EXPLORER, edited by R. Randy Ray. 
This month's column is titled "Seismic Meta Attributes as a Practical 
Exploration Tool: Gas Chimney and Fault Volumes."
Looking For Gas Chimneys And Faults

Editor's note: Fred Aminzadeh is president of dGB-USA, Houston 
(www.dgbusa.com); David Connolly is the chief geologist at dGB-USA.
Click to enlarge image.

FIGURE 1

FIGURE 2

FIGURE 3

FIGURE 4

FIGURE 5

FIGURE 6
Gas chimney and fault volumes extracted from 3-D seismic data are rapidly 
becoming valuable tools for exploration and field development. Various 
seismic anomalies such as chimneys, faults, fractures, salt and sand 
bodies can be highlighted using a new technique that analyzes data with 
combinations of seismic attributes.
This article focuses on the mapping of gas chimneys and faults; a 
forthcoming column will illustrate the detection of salt bodies and 
channel sands. 
New Type of Seismic Volumes
Chimney cubes (figure 1) and fault cubes (figure 2) are used to map areas where the 
seismic detects anomalous patterns of 
amplitude and similarity in combination with other attributes like dip 
variance and curvature. They help determine where hydrocarbons originated, 
how they migrated into a prospect and where they leaked, creating shallow 
gas (and sometimes mud volcanoes, or pockmarks) at the sea floor.
Current applications of chimney and fault cubes include:
Unraveling a basin's migration history. 
Distinguishing between charged and non-charged prospects. 
Distinguishing between sealing versus non-sealing faults. 
Determining vertical migration of gas. 
Identifying potential for over-pressure. 
Detecting shallow hazards. 
Predicting hydrocarbon phase and charge efficiency, especially in 
multiphase petroleum systems. 
Computers can be trained to search through data volumes looking for 
seismic objects using carefully designed criteria "meta-attributes," which 
are an aggregation of a number of seismic attributes where the 
interpreter's insight is combined with the power of a trained neural 
network to detect a particular seismic anomaly.
As shown in figure 3, a multitude of attributes from known or suspected chimneys (or 
faults) 
are used as input to a neural network.
Training of the neural network using interpreter's insight renders the 
"meta-attribute" suitable for detection of a given seismic body, like gas 
chimneys or fault patterns. 
Gas Chimney
Figure 1 shows a typical gas chimney in yellow overlaid on a deep salt structure 
with deep and shallow reservoir units. It highlights the migration pathway 
of hydrocarbon from deep structures into shallower reservoirs and into 
near surface gas pockets.
Gas clouds and gas chimneys have often been considered as a source of 
seismic noise that degrades the quality of seismic reflection events. Much 
effort has been devoted to filter out the impact of gas clouds and provide 
interpretable sections by imaging through them.
Our main focus, however, is to highlight such events and establish a link 
between chimney characteristics (occurrence, type and extent) and geologic 
concepts critical for successful exploration.
For example, mapping the location and origination/termination points of 
gas chimneys helps the:
Understanding of deep petroleum migration processes. 
Distinguishing between charged and non-charged fault segments. 
Detecting sealing versus leaking faults. 
Distinguishing oil-prone versus gas-prone prospects. 
Sometimes it is difficult to pinpoint deep migration pathways on a 
conventional seismic line -- but chimney cubes can highlight subtle 
features like vertical gas migration in the geo-pressured sections of the 
Gulf of Mexico. This helps substantiate predictions of geochemists and 
geologists that vertical migration is an important process in charging 
Tertiary reservoirs in the Gulf of Mexico and in other similar basins 
around the world.
Chimney and fault volumes improve the understanding of the petroleum 
system and identify the role faults play in the migration of hydrocarbons 
into the reservoir.
Distinguishing Charged Fault Segments
In figure 4 we have overlaid the chimney halo (in orange) on top of the seismic 
section.
Note that the two structures on opposite sides of the fault have similar 
seismic response but very different charge probability.
The structure on the right side of the fault has no chimney halo 
associated with it, and thus is less likely to be charged. In general, 
structures with some associated strain possess preferential charging 
potential.
Of course, we have to keep in mind that excessive strain would be a major 
leak risk, so chimney analysis should be used in conjunction with other 
tools which predict stress/strain regimes.
Sealing vs. Leaking Faults
Combining fault and gas chimney data can be a powerful tool in detecting 
hydrocarbon migration pathways. Figure 5 shows their use in determining sealing versus 
leaking faults.
While all the mapped faults are highlighted in Figure 5b, the subset of the faults 
that are likely to be leaking show up in the 
chimney volume of Figure 5a. This information can then be integrated with other 
regional information 
to assess probability for hydrocarbon charge and seal.
Many fields in the Gulf of Mexico and other basins demonstrate that the 
fault systems associated with gas chimneys have been major charging 
pathways for the reservoirs. Figure 6 shows active chimneys (in yellow), both large 
(e.g. one at the 
intersection of the two lines) and small (along selected fault blocks) 
that are considered to be leaking.
Presence of chimney-like behavior along faults can indicate evidence of 
vertical hydrocarbon movement. 
Oil-Prone vs. Gas-Prone Prospects
In multi-phase petroleum systems, where both oil and gas are migrating 
into a trap, the structures that vent the gas (either through faulting or 
fractures) will be more oil-prone. Processing can detect the weak signal 
associated with venting.
This approach has been used to successfully predict hydrocarbon phase in a 
number of basins in West Africa, the North Sea, GOM and the Far East. 
Based on worldwide case histories from gas prone basins, chimney and fault 
cube analysis is a proven tool to make geologic predictions. This 
includes:
Relating surface seeps to subsurface structures and reservoirs. 
Understanding the hydrocarbon history model. 
Ranking prospects. 
Detecting reservoir leakage and spill points. 
Assisting in identifying potential over-pressured zones and shallow gas 
drilling hazards. 
Assessing the sea floor stability for platform design and drilling. 


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