A Cenozoic Tectonic Model for Southeast Asia - Microplates and Basins
Kevin A. Maher
A computer-assisted Cenozoic tectonic model was built for Southeast Asia and
used to construct 23 base maps 2 to 6 million years apart. This close temporal
spacing was necessary to explain all the local geometric
shifts in a consistent
and geologically feasible fashion. More than a hundred individual blocks were
required to adequately treat Cenozoic microplate processes at a basic level. The
reconstructions show tectonic evolution to be characterized by long periods of
gradual evolution, interrupted by brief, widespread episodes of reorganization
in fundamental plate geometries and kinematics.
The model takes into account difficulties inherent in the region. First, the
Pacific and Indo-Australian plates and predecessors have driven westward and
northward since the late Paleozoic, towards each other and the relatively
stationary backstop of Asia. Southeast Asia is therefore the result of a
long-lived, complex process of convergent tectonics, compounding the difficulty
of reconstructing tectonic development. This history of subduction and collision
erased much of the continental margin and sea floor spreading
record. In
addition, convergent tectonic regimes are dominated by small-scale microplate
processes with short time scales and internal deformation, taking place in
rapidly evolving and more ductile buffer zones between the major rigid plate
systems. These relatively ephe eral crustal blocks appear and die within the
plate interaction zones, or accrete to and disperse from the margins of the
major plate systems. Such microplate evolution is the dominant factor in
Cenozoic basin evolution.
This detailed tectonic model aids in comprehension and prediction of basin development and hydrocarbon habitat.
AAPG Search and Discovery Article #91020©1995 AAPG Annual Convention, Houston, Texas, May 5-8, 1995