--> Abstract: A Cenozoic Tectonic Model for Southeast Asia: Microplates and Basins, by K. A. Maher; #90958 (1995).
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Abstract: 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 constrain all the local Previous HitgeometricNext Hit 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. These episodes are triggered by major collisions, or by accumulation of smaller changes.

The model takes into account difficulties inherent in the region. The Pacific and Indo-Australian plates and their 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, making it difficult to reconstruct tectonic evolution as much of the continental margin and sea floor Previous HitspreadingTop record was erased. In addition, the region has been 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 plate interaction zones have taken up much of the relative motion between t e major plates. Relatively ephemeral crustal blocks appear and die within the buffer zones, or accrete to and disperse from the margins of the major plate systems. However, such microplate evolution is the dominant factor in Cenozoic basin evolution.

This detailed tectonic model aids in comprehension and prediction of basin development, regional hydrocarbon habitat, and petroleum systems.

AAPG Search and Discovery Article #90958©1995 AAPG Pacific Section Meeting, San Francisco, California