Molucca Sea Plate

Molucca Sea Plate
Type Minor
Movement1 ?
Speed1 ?
Features Molucca Sea
1Relative to the African Plate

Earlier theory

The Molucca Sea Plate (also Molucca Sea Microplate) was theorised to be a small tectonic plate carrying northern Sulawesi, the Molucca Sea and a portion of the Banda Sea in a region littered with numerous small plates. The theory suggested a subduction zone lies along its northern border with the Sunda Plate. A small divergent boundary exists along the Sulawesi part of the border with the Banda Sea Plate and transitions into a convergent boundary as it bisects the Banda Sea; the rest of the borders being transform boundaries.

Current theory

More recent scientific studies suggest the Molucca Sea Plate has been totally subsumed by the Halmahera Plate and the Sangihe Plate, so that no portion of the Molucca Sea Plate remains exposed to Earth's surface. The tectonic setting of this region is unique in that it is the only global example of an active arc-arc collision consuming an oceanic basin via subduction in two directions, between microplates Halmahera Plate and Sangihe Plate.[1] To the Southeast is the Sorong Fault, a major lateral east-west fault in the region which separates Bird's Head Plate and Halmahera Plate. This theory is more fully discussed in the article Molucca Sea Collision Zone.

Large earthquakes frequently strike this area sometimes triggering tsunamis.

Recent large quakes (>6.0) in region

[2]

References

This article is issued from Wikipedia - version of the Monday, January 11, 2016. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.