Page 255 - Carbonate Platforms Facies, Sequences, and Evolution

240
Table 2.
9
19
21
Locality
Acatita
3 La Mula
Block E
Sierra de
Poza Rica
Teran well
Tamaulipas
10 Linares well
20 Tepehauje 2
17 San Rafael 2
13 Papaya 1-A
Las Delicias­
7 Pecten 1 well
15 Arroyo Viejo
16 Punta Jerez 5
11 Arenque field
4 Menchaca well
8 Benmerito well
14 Juana Ramirez
Tezuitlan block
Tezuitlan block
Sabinas Hidalgo
5 Monclova 5 well
18 Barreta 2 SW of
Camotal 1 and 2
north of Block E
northern Block E
2 Sierra De Mojado
12 Muleto (Block E)
Ojital 101 south of
6 Anahuac field wells
Schist
Gneiss
Granite
Granite
Granite
Granite
Granite
Granite
Granite
Granite
Granite
Areas of presumed Triassic granitic intrusions
Granodiorite
Granodiorite
conglomerate
pluton is tonalite
Granite basement
clastics over schist
Petrography
Granite boulders in
strike with La Mula
Altered granodiorite
'Granite basement'?
Fossiliferous Permian
Granite-Granodiorite
J.L. Wilson
Intrusive igneous rock on
Granodiorite, Las Delicias
273
320
183
1984)
1984)
1972)
(1969)
redbeds
reference
reference
Leonardian
Sanchez, 1982)
(Mississippian)
above reference
above reference
above reference.
183 Ma (Liassic?)
et al. , 1984, 1988)
Ma (Liassic?)
162Ma (mid-Jur.)
(Jones et al., 1984)
Wilson et al. (1984)
234 Ma (late Permian)
Under Upper Jurassic
Penn. intrusions during
Ma above reference
Rivera (1976 in Padilla y
212 Ma±5 (Permo-Trias)
Alfonso-Zwanziger (1978),
rocks. Possibility of Permo­
Triassic batholith intrusion
caused by heating owing to
139±9Ma Rb/Sr (late Jur.)
192±3 (late Triassic) above
210Ma (late Trias.) Date is
1970) Late Trias, cuts Penn.
208Ma K/Ar (Denison et al.
204 Ma Shell; 211-213 Trias
225Ma Permo-Trias (McKee
Pre-Huizachal (Wilson et al.,
Pre-Huizachal (Wilson et al.,
deposition also exists. Canon
184±14 Rb/Sr (Lias?) above
Rosillo volcanic sediments are
Age and evidence, (method of
± 5 (Permo-Carboniferous)
dating indicated where known)
Under 137m of Upper Jurassic
below Up. Jur. (Lopez-Ramos,
237±5 (Permian) Denison et al.
Eocene date for granite which is