Burma Plate

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The Burma Plate, showing boundaries with the India Plate (the Sunda Trench) and the Sunda Plate (through the Andaman Sea)

The Burma Plate is a small tectonic plate or microplate located in Southeast Asia, often considered a part of the larger Eurasian Plate. The Andaman Islands, Nicobar Islands, and northwestern Sumatra are located on the plate. This island arc separates the Andaman Sea from the main Indian Ocean to the west.

To its east lies the Sunda Plate, from which it is separated along a transform boundary, running in a rough north-south line through the Andaman Sea. This boundary between the Burma and Sunda plates is a marginal seafloor spreading centre, which has led to the opening up of the Andaman Sea (from a southerly direction) by "pushing out" the Andaman-Nicobar-Sumatra island arc from mainland Asia, a process which began in earnest approximately 4 million years ago.

To the west is the much larger India Plate, which is subducting beneath the eastern facet of the Burma Plate. This extensive subduction zone has formed the Sunda Trench.

Tectonic history[edit]

In models of the reconstructed tectonic history of the area, the generally northwards movement of the Indo-Australian Plate resulted in its substantive collision with the Eurasian continent, which began during the Eocene epoch, approximately 50-55 million years ago (Ma). This collision of the India Plate portion with Asia began the orogenic uplift which has formed the Himalaya mountains.

As the India Plate drifted northwards at a relatively rapid rate of an average 16 cm/yr, it also rotated in an counterclockwise direction. As a result of this movement and rotation, the convergence along the plate's eastern boundary (the Burma-Andaman-Malay region) with Eurasia was at an oblique angle.

The transform forces along this subduction front started the clockwise bending of the Sunda arc; in the late Oligocene (ca. 32 Ma) further faulting developed and the Burma and Sunda microplates began to "break off" from the larger Eurasian plate.

After a further series of transform faulting, and the continuing subduction of the India Plate beneath the Burma plate, backarc spreading saw the formation of the marginal basin and seafloor spreading centre which would become the Andaman Sea, a process well-underway by the mid-Pliocene (3-4 Ma).

Western Sunda Arc and Trench showing tectonic and seismic activity.

Recent tectonic activity[edit]

On December 26, 2004, a large portion of the boundary between the Burma Plate and the Indo-Australian Plate slipped, causing the 2004 Indian Ocean earthquake. This megathrust earthquake had a magnitude estimated by researchers to be between Mw9.0 and Mw9.3.[1] Over 1600 km of the boundary underwent thrust faulting and shifted up to 5 meters vertically and 11 meters horizontally.[1] This rise in the sea floor over such a short time (seven minutes[1]) generated a massive tsunami that killed approximately 229,800 people along the coast of the Indian Ocean.

References[edit]

  1. ^ a b c Strand, Carl; John Masek (2008). Sumatra-Andaman Islands earthquake and tsunami of December 26, 2004 : lifeline performance. Reston, Va.: American Society of Civil Engineers. ISBN 9780784409510.