Sunda Craton

E565330

The Sunda Craton is an ancient, stable block of continental crust in Southeast Asia that underlies much of the region’s landmass and adjacent shallow seas.

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All labels observed (1)

Label Occurrences
Sunda Craton canonical 1

Statements (44)

Predicate Object
instanceOf craton
alsoKnownAs Sundaland NERFINISHED
Sundaland Craton NERFINISHED
associatedWith Sunda Shelf sea-level changes
exposed land bridges during Pleistocene low sea level
boundedBy Sunda Arc subduction zones NERFINISHED
tectonically active margins of Indonesia
characterizedBy ancient continental crust
tectonic stability
continent Asia
formedBefore Mesozoic era
formsPartOf Southeast Asian continental core
hasCrustType thick continental crust
hasEconomicImportance mineral resources
natural gas resources
petroleum resources
hasFeature broad shallow continental shelf
relatively low seismicity compared to surrounding arcs
hasGeologicalAge Precambrian core
hasLithosphereType continental lithosphere
hasPaleogeographicName Sundaland NERFINISHED
importantFor biogeographic history of Southeast Asia
hydrocarbon accumulation in Southeast Asia
paleogeographic reconstructions of Southeast Asia
influences regional sea-level response and coastline position
locatedInRegion Southeast Asia NERFINISHED
overlainBy Cenozoic sedimentary basins
Mesozoic sedimentary basins
partOf Eurasian Plate NERFINISHED
playsRoleIn configuration of Southeast Asian continental shelves
distribution of terrestrial fauna in Sundaland
relatedTo Indochina Block NERFINISHED
South China Block NERFINISHED
studiedInDiscipline geology
plate tectonics
tectonics
underlies Borneo NERFINISHED
Java Sea NERFINISHED
Malay Peninsula NERFINISHED
South China Sea shelf areas NERFINISHED
Sumatra NERFINISHED
Sunda Shelf NERFINISHED
adjacent shallow seas of Southeast Asia
much of the Southeast Asian landmass

Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.

Sunda Shelf partOf Sunda Craton