3c Proposal 1
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Transcript of 3c Proposal 1
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A Brief Introduction
For
Multi-Component Seismic Data Processing
ubmitted byBGP Jakarta Data Processing Center
January 16, 2006
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1. Introduction
BGP Jakarta Data Processing Center is fully supported by Geophysical Research
Institute (GRI) of BGP, China GRI is a reputed international Geophysical ser!ices
co"pany ha!ing !ery sound research and de!elop"ent background in Geophysical
industry It has e"ployed and de!eloped highly ad!anced technologies and therefore
has beco"e a #orld le!el ser!ice and research co"pany in geophysical prospecting
industry
$he data #as processed using PR%&',G%DP$* and GRI++ as the "ain
Geophysical application processing soft#are (!ersion -.), #hich #as de!eloped by
GRI of BGP In addition to GB++ seis"ic processing soft#are for pre/stack ti"e
"igration de!eloped by Globe Co"pany of *ouston 0+' is also a!ailable $he
seis"ic application soft#are package is co"prised of se!eral geophysical data
processing "odules, #hich are capable of undertaking full 1D and 2D interacti!e and
batch processing functions
Data Processing Center Page 2
Since 1983 BGP has experimented and developed multi-componenttechnology !his expertise has evolved into a series o" integratedtechni#ues $hich have %een tested and have proved to %e relia%le suite o"exploration and development seismic services
&ntegrated !echni#ues
' component processingStaticsPre-stack noise attenuationSurface consistent processingVelocity analysis, NMO, stackImaging
' component processingStaticsPre-stack noise attenuationSurface consistent processingVelocity analysis, NMO, stackImaging
()* component processingS wave staticsCCP binningP-SV velocity analysisP-SV wave NMOP-SV wave imaging!traction of attributes
()* component processingS wave staticsCCP binningP-SV velocity analysisP-SV wave NMOP-SV wave imaging!traction of attributes
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Data Processing Center Page 3
%e"ore
a"ter
S-$ave Statics
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Data Processing Center Page
Conventional +, +on-hyper%olic +,Super gather
PS. +,
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Data Processing Center Page !
P-P
PSV
/ithology prediction using .p0.s ratio
Gas-%earing sandstone
inal processing results
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2. 3 Component Seismic Data Processing
1. "e#uired input data
3e #ill re4uest C%&P'5 #ith the follo#ing data6
1D 2C 7ield seis"ic tapes (!ibroseis correlated) and additional data (obser!erreport, coordinates and ele!ations (+P+), uphole data)
P/#a!e !elocity "odel fro" anisotropic pre/stack ti"e or depth "igration of
P/P #a!e data (depth "aps, !elocity file, 8$I para"eters)
7inal processing results of P/P #a!e data
3ell data
%ther data re4uired for data processing
2. Pre-Processing and Preparations
9 Data loading2 +hot gathers and all near traces display
1 Geo"etry updating6 $he geo"etry can be defined #ith +P+ file $he linear
5&% and shot gathers displays #ill be perfor"ed to check the result of the
defined geo"etry
2 Co"ponent separation6 8, *9, *1
: Construction of a 8p;8s (9/D) background "odel fro" 8+P and;or #ell log
data
3. P-P $a%e Processing
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. Poststac' processing (for PP and PS)
12 Decon!olution after stack >C products
1: $i"e !ariant filter >C products
1C products
1- 7/ decon!olution1= $i"e !ariant gain >C products
1? Phase analysis, phase shift6 ero/phasing filter to be deri!ed statistically or by
"atching the seis"ic to a supplied #ell reflection series >C products
1@ Generation of final deli!erables
!. P-S $a%e Processing
7or the processing of the horiontal co"ponents, a "odification of the P/P #a!e
processing #ill be applied Differently fro" P/P #a!e processing there are no
restrictions of "ai"u" offset or trace length (data as ac4uired shall be used)
'dditional steps or "odifications of steps are6
2. Restriction of "ai"u" offset to < k"
29 5egati!e offset polarity re!ersal, re!erse trace analysis and correction +hot
gathers and all near traces #ill be displayed &aps sho#ing the a"plitude of
the signal and noise at !arious ti"es in the data set
21 Rotation analysis and tests >C products
22 P/#a!e and +/ #a!e static >C products
2: 7irst Break Picking ("anually and;or auto"atically), Refraction +tatic
Co"putation and Refraction +tatic 'pplication >C products
2C products
2- CCP operations instead of C&P operations >C products
2= In!erse >s filter >s to be calculated by esti"ating the spectral change #ith
different ti"e +uited >C plots for testing and application
2? %ffset separation (positi!e and negati!e offsets) prior to P+$&
2@ Airchoff pre/stack ti"e "igration( para"eter tests, >C plots)
:. 5&% in!erse using Airchoff
:9 P+$& !elocity analysis
:1 Airchoff pre/stack ti"e "igration
:2 5&% in!erse
:: *igher order 5&%, "ute and +tack
&. 0ptional + additional Processing
:C products
:- *igher order non/hyperbolic 5&% corrections >C products
:= $ri" statics >C products
:? 7D &igration #ith P+ a!erage !elocities (1E8p8s;(8pF8s)) >C products
:@ Generation of +P+
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"ethod to be applied +uited >C products6 prestack and stack gathers before ;
after
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. /,e Proposed Flo C,art of t,e 2D Seismic Data Processing
81 P-P 2ave Basic Processing Se#uence
Demultiplexing
Shot Gathers Display
Geometry pdate
Sort to .ertical Component
4dit %ad traces0shots) de-spi5ing
4levation Static Correction
irst Brea5 Pic5ing) 6e"raction Static Correction
Spherical Divergence Correction
Sur"ace consistent amplitude compensation
Sur"ace consistent deconvolution
Sort to C,P gather
irst pass velocity analysis 7every m: and stac5
irst Pass Sur"ace Consistent 6esidual Statics Correction
Predictive Deconvolution or &nverse ;-"ilter
Second pass velocity analysis 7every
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-( deconvolution
Post-stac5 Deconvolution
!ime variant "ilter
Scaling
inal 6esult
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8< P-S 2ave Basic Processing Se#uence
Demultiplexing
Shot Gather and +ear ""set Display
Geometry pdate
irst Brea5 Pic5ing) 6e"raction Static Correction
Sort to ?ori@ontal Component
Construction o" a .p0.s
+egative o""set polarity reversal) reverse trace analysis and correction
6otation analysis and tests
PS static application
4dit %ad traces0shots) de-spi5ing
= ilter at Shot06eceiver Domain7ptional:
Spherical Divergence Correct
Sur"ace consistent amplitude compensation
Sur"ace consistent deconvolution
Sort to CCP
CCP velocity analysis 7every m: and stac5
1stSur"ace Consistent 6esidual statics Correction
Predictive Deconvolution or &nverse ;s-"ilter
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!hird Pass .elocity >nalysis
=irchho"" Pre-stac5 !ime ,igration
+, &nverse and S4G* 6>2 PS!, Gather
+,) ,ute and Stac5
-( deconvolution
Post-stac5 Deconvolution
!ime variant "ilter
Scaling
inal 6esult
4. 6e7 processing tec,ni#ues for Multi-Component Seismic Data
Automatic *p+*s Pic'er
Co-Sensor Interpolation
Co-Sensor Sum
Common Con%ersion Point (CCP) Binning
Multi-Component Cross-8#uali9ation
S-$a%e 2-Component "otation
*p+*s Computation
*p+*s Correlation
*p+*s /ransform
P-S% PS/M
P-S% DM0
15. 6e7 Processing /ec,nic Description
Common Con%ersion Point (CCP) Binning
Pre/stack P/+ con!erted #a!e data are rebinned to co""on con!ersion point (CCP)
location instead of co""on "idpoint (C&P) location for subse4uent processing ach
input trace is seg"ented into user/specified ti"e #indo#s that are indi!idually
rebinned and output as ne# traces 8elocity "anager for"atted files of !elocities and
of 8p;8s ratios are re4uired
Multi-component Cross-8#uali9ation
7or land and "arine "ulti/co"ponent data, this "odule cross/e4ualies the a"plitude
and phase spectra of the horiontal detector co"ponents for opti"al !ector #a!efield
processing, including co"bination (rotation) using the +/3a!e 1/co"ponent Rotation"odule $he !ertical detector co"ponent "ay be included in the co"putation and
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"ay also be corrected to re"o!e spurious +/#a!e energy
S-$a%e 2-Component "otation
7or land and "arine "ulti/co"ponent data, the horiontal detector co"ponents of
shear/#a!e data are rotated to obtain the desired #a!efield $he data "ay be rotated
to the source/detector direction, a co""on direction, or back to the original directionIf the original field orientations of the horiontal co"ponents are not kno#n, they
"ay be calculated so that subse4uent rotation can be perfor"ed
*p+*s /ransform
+tacked co"pressional/#a!e, con!erted/#a!e, or shear/#a!e reflection data t#o/#ay
tra!elti"es are transfor"ed to t#o/#ay tra!elti"es of a different type By correlating
a transfor"ed !ersion of one #a!e type to a recorded !ersion of that #a!e type, an
analysis of the ratio of co"pressional/#a!e !elocity (8p) to shear/#a!e !elocity (8s)
can be "ade $his can aid in the interpretation of lithology and fluid properties fro"
seis"ic data Input data is post/stack and trace selected as re4uired %utput can be a
transfor"ed stack fro" a!erage 8p;8s function or a set of transfor"ed gathers, useful
for 8p;8s correlation analysis ' co"plete input trace or a single #indo# of data can
be transfor"ed
P-S* DM0
P/+8 D&% is perfor"ed #ith a space/ti"e (/t) Airchhoff algorith" $he input data
are co""on/offset gathers #hich ha!e not been 5&% %utput obtained that consists
of co""on/offset gathers #hich approi"ate P/P data in an e4ui!alent !elocity
"ediu" 'dditional processing, such as a residual 5&% correction, is typically
re4uired after applying this process
11. Final Products
+G tapes of the PP and P+ final stack and "igration
+G tapes of final filtered ero/phased PP and P+ "igration
PP and P+ P+$& or D&% gather tapes in +G
PP and P+ stacking and "igration !elocities in '+CII for"at
+G tape of final 8p;8s sections
7inal report (2 paper copies plus 2 CDR%& PD7 file copies)
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Data Processing Center Page 1