Continental crustal fragments, partly with microcontinents,["Microcontinent" was initially the broader term, because it was defined morphologically rather than genetically (in terms of genesis or origin). Scrutton, Roger A. (1976) "Microcontinents and Their Significance" pp. 177–189 In Drake, Charles L. (1976) (editor) Geodynamics: Progress and Prospects American Geophysical Union, Washington, D.C., . But, using Scrutton's definition, "microcontinent" is a narrower term, excluding aseismic ridges of continental material, such as the Lomonosov Ridge and the Jan Mayen Ridge, which could still be considered "continental fragments".] are pieces of that have broken off from main continental masses to form distinct islands that are often several hundred kilometers from their place of origin.
Causes
Continental fragments and microcontinent crustal compositions are very similar to those of regular continental crust. The rifting process that caused the continental fragments to form most likely impacts their layers and overall thickness along with the addition of
mafic intrusions to the crust. Studies have determined that the average crustal thickness of continental fragments is approximately .
The
Sediment of continental fragments can be up to thick and can overlay two to three crustal layers. Continental fragments have an average crustal density of which is very similar to that of typical continental crust.
Strike-slip fault zones cause the fragmentation of microcontinents. The zones link the extensional zones where continental pieces are already isolated through the remaining continental bridges. Additionally, they facilitate quick crustal thinning across narrow zones and near-vertical strike-slip-dominated faults. They develop Fault block patterns that slice the portion of continent into detachable slivers. The continental fragments are located at various angles from their .
History
Some microcontinents are fragments of
Gondwana or other ancient
continents; examples include Madagascar; the northern Mascarene Plateau, which includes the Seychelles Microcontinent; and the island of
Timor.
Other islands, such as several in the
Caribbean Sea, are composed largely of granitic rock as well, but all continents contain both granitic and basaltic crust, and there is no clear dividing line between islands and microcontinents under such a definition. The Kerguelen Plateau is a large igneous province formed by a volcanic hotspot; however, it was associated with the breakup of
Gondwana and was for a time above water, so it is considered a microcontinent, though not a continental fragment.
[ UT Austin scientist plays major rule in study of underwater "micro-continent". Retrieved on 2007-07-03][ Sci/Tech 'Lost continent' discovered Retrieved on 2007-07-03] Other hotspot islands such as the
Hawaiian Islands and Iceland are considered neither microcontinents nor continental fragments. Not all islands can be considered microcontinents:
Borneo, the
British Isles, Newfoundland, and
Sri Lanka, for example, are each within the continental shelf of an adjacent continent, separated from the mainland by inland seas flooding its margins.
Several islands in the eastern Indonesian Archipelago are considered continental fragments, although this designation is controversial. The archipelago is home to numerous microcontinents with complex geology and tectonics. This makes it complicated to classify landmasses and determine causation for the formation of the landmass.
List of continental fragments and microcontinents
Continental fragments (pieces of Pangaea smaller than Australia)
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Parts of
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Possibly Sumba, Timor, and other islands of eastern Indonesia; Sulawesi formed via the subduction of a microcontinent
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South Orkney microcontinent
Other microcontinents (formed post-Pangaea)
Future microcontinents
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Ajan, a continent that will form in 3 to 20 million years time because of its breakoff with mainland Africa.
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Davis Strait proto-microcontinent, Currently in the process of forming between Greenland and Canada.
See also
