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Abstract
Mexico
: Subsurface and Outcrop
Studiesfrom:
Mexico
Basin: Tectonics, Sedimentary
Basins, and Petroleum SystemsThe Taraises Formation (Berriasian-Valanginian) in
Northeastern
Mexico
: Subsurface and Outcrop Studies
Abelardo Cant
-Chapa
Instituto Polit
cnico Nacional,
Mexico
City,
Mexico
ABSTRACT
Mexico
consists of an intercalation of argillaceous limestone and shale. This formation is
divided into two members, based on lithologic characteristics defined from electric and
radioactivity logs from oil wells in northeastern
Mexico
. In addition, two small ammonite
groups of the subfamily Olcostephaninae (upper Valanginian) collected at Potrero de Garc
a, Nuevo Le
n, northeastern
Mexico
, are described: (1) Capeloites neoleonense n. sp. and (2) Garcites
potrerensis n. gen. and sp. and G. cavernensis n. gen. and sp. The
presence of Dichotomites (Dichotomites) sp. in the same beds supports an
late Valanginian age for these strata. One specimen of Capeloites obtained from a
core of the La Laja-8 well, south of Tampico City, eastern
Mexico
, designates an late
Valanginian age for the interval drilled (2556-2562 m) in the so-called Lower Tamaulipas
Formation in this area. Global geographic distribution of Capeloites is
restricted to France, Spain, and Peru; its presence in
Mexico
supports a biogeographic
link between Europe and America.
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