MC Prestack Joint Inversion S-Impedance Result
Discussion
Extensional Fractures
MESOZOIC
Mosquera and Ramos (2005)
AGE
CENOZOIC
TERTIARY
CRETACEOUS
EARLY
PLIOCENE
VOLCANICS
MOCENE
PROGINIC TERARY
NAZCA STAGE
BROKEN FORELAND BASIN
70°
LATE FARALLON STAGE
CONVERGENCE
DIRECTION (°)
FORELAND BASIN
MALARQUE OR
100°
ALBOCENE
Campanan
Santonian
Cortacan
NEJOVEN G
Turonian
Cenomanian
312
Guzmán et al. (2011)
Volcanic
Abun
TAYOSO Fm.
UPPER CRETACEOUS
PALEOCENE
EARLY FARALLON STAGE
INTRAPLATE DEFORMATION
La Txa
100°
AT
Barrenian
TRAATIAN
Up
Choneado
Upper Mt
Aye Ma
Kautanvan
Lower M
Katanginan
Sinistral convergence> 45
2324
STALINA
285°
MA
Bemasan
Tithenian
QUINTUCO
VICA MUERTA
Oxfordian
Callovian
Fms
TOROLLO FRAMES
AUQUALCO F
LA MANGA P
LOTENA FRACAS
ALUK STAGE
INTRAPLATE DEFORMATION
140°
Toarcun
LOS MOLLES
FM
Persbachian
INTRALASI
Sinistral convergence-45
pper br
Lower Mar
RIFT STAGE
Nortan
Caran
CHOYCE G
LITHOLOGIC COLUMN
LHOESTRATIGRAFIC REGINAL
UNT UNCONS
BASIN EVOLUTION STAGE
255
240
300°
2250
65%
Bitumen
Dikes
EOCENE
Dikes
50°
76
90°
Well
Breakouts
OLIGOCENE
MIOCENE
PLIO.Q
Middle MVM - Well G
9°
345
15%
330°
nd
30°
9%
Set
315°
45
49
135
120°
60°
75°
105
90
RCP0
In pursuit of new ideas
2100
150°
1st Set
195°
165°
123
180°View entire presentation