Print this pageReactivation of Mesozoic Age Structures Near La Ceiba Field, NE Anzoategui, Eastern Venezuelan Basin
WHITE, STAN, and PETER SADLER
The structural style of this portion of the Eastern Venezuelan basin is
dominated by reverse and low angle faults and their associated folded and
faulted strata. Structural development is related to inversion of Mesozoic age
extensional faults during the Miocene. La Ceiba field is located at the western
termination of the Tala-Pirital thrust 
fault
system. Miocene structural
reactivation was in response to oblique convergence between the Caribbean and
South American plates. First order structural features effected by Miocene
structuring include the NE-oriented Anaco fault, the ENE-oriented Tala fault,
and the NW-oriented Urica fault zone.
Using seismic data, three phases of Late Oligocene to Miocene age structuring have been identified. The first was extensional and involved reactivation of Mesozoic age normal faults. This resulted in both regional and local increased accommodation for late Oligocene and Lower Miocene sedimentation. Secondly, regional inversion along the Anaco and related structures followed extension in Middle to Upper Miocene time. Thirdly, breakthrough and emplacement of the Tala thrust system east of La Ceiba field took place.
Oil and gas production at La Ceiba field is localized by structure that
developed at the western termination of the Tala thrust. There it is recognized
to be at the juncture of the NE limit of the Anaco fault
and NW oriented
compressional splays of the Tala thrust.