This is the most common pelagic sediment by area, covering 48 % of the world ocean's floor.
12.
The formation of the Cordillera Oriental covered the continental platform with pelagic sediments with Precambrian and Paleozoic metamorphic rocks bases.
13.
This theory holds due to evidence of pelagic sediments and continental crust being subducted in processes known as sediment subduction and subduction erosion respectively.
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It accumulates more rapidly than any other pelagic sediment type, with a rate that varies from 0.3 5 cm / 1000 yr.
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North of 50?south latitude, 86 % of the main basin is covered by pelagic sediments, of which more than half is globigerina ooze.
16.
Filling spaces in between the pillows in the pillow lava units are dispersed metal oxide sediments that can also be seen as carbonates, volcanic glass and pelagic sediments.
17.
Subducting slabs are composed of basaltic crust topped with pelagic sediments; however, the pelagic sediments may be accreted onto the forearc-hanging wall and not subducted.
18.
Subducting slabs are composed of basaltic crust topped with pelagic sediments; however, the pelagic sediments may be accreted onto the forearc-hanging wall and not subducted.
19.
This is also supported by geological evidence : 200-230 Ma granite in Lincang, near the Changning-Menglian suture, indicate a continent-continent collision occurred there in the Late Triassic; pelagic sediments in the Changning-Menglian-Inthanon ophiolite belt ( between Sibumasu and Indochina ) ranges in age from Middle Devonian to Middle Triassic, while, in the Inthanon suture, in contrast, Middle to Late Triassic rocks are non-pelagic with radiolaran cherts and turbidic clastics indicating the two blocks had at least approached each other by that time; volcanic sequences from the Lancangjiang igneous zone indicate a post-collisional setting had developed before the eruptions there around 210 Ma; and, the Sibumasu fauna developed from a non-marine peri-Gondwanan assemblage in the early Permian, to an endemic Sibumasu fauna in the Middle Permian, and to an Equatorial-Cathaysian in the Late Permian.
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