MC Prestack Joint Inversion S-Impedance Result
Discussion
• Expulsion of Hydrocarbon.
Jurmsic
MESOZOIC
Mosquera and Ramos (2005)
AGE
CENOZOIC
TERBARY
CRETACEOUS
EARLY
LATE
PLIOCENE
VOLCANCS
NAZCA STAGE
BROKEN FORELAND BASIN
70°
MOCEME
DROGEN TERSARY
PALBOCENE
MALARGUE GR
Campanan
Samman
LATE FARALLON STAGE
FORELAND BASIN
100%
Turonian
Cenomanan
AD 31
NEUQUEN G
AFT
RAYOSO FM
EARLY FARALLON STAGE
NTRAPLATE DEFORMATION
La Ta
100%
TOE 10 AN
Chamad
Mb
300°
Samman
Upper M
Ave M
Hauteman
Lower
atanginan
Bemason
Tithonian
QUINTUCO+
Fms
Oxfordian
AUQUELCO P
Callevian
LAMANGA P
PAJAL T
அம்
Tuartian
LOS MOLLES
Fm
Persbechin
Upper
Lower M
Carna
CHOVYOIG
Sinistral convergence> 45°
ALUK STAGE
INTRAPLATE DEFORMATION
Sinistral convergence-45
RIFT STAGE
LITHOLOGIC COLUMN
LHOESTRATIGRAFIC REGINAL
BASIN EVOLUTION STAGE
CONOS
140
2559
285
240
225°
3159
Middle MVM - Well G
0°
345°
15°
330
30°°
996
496
210
150°
1959
165
1900
135°
120
600
105
780
RCP0
In pursuit of new ideas
125View entire presentation