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Compositions of sandstones in circum-Pacific subduction complexes and fore-arc basins

Journal Article · · Am. Assoc. Pet. Geol., Bull.; (United States)
OSTI ID:5361202

Arc-trench systems of the circum-Pacific orogenic belt contain voluminous sandstones within fore-arc terranes that include complexly deformed fore-arc basins of several types. Turbidites incorporated within subduction complexes include not only axially transported trench fill, but also abyssal-plain sediments deposited on the sea floor beyond the trench, and slope-basin deposits perched on the accretionary trench slope. Mean framework modes of circum-Pacific sandstone suites can be expressed adequately by the use of QFL and QmFLt plots. Supplementary QmPK and QpLvLs plots depict partial modes of mineral grains alone and polycrystalline lithic fragments, respectively. Source rocks were mainly volcanic and plutonic terranes of the circum-Pacific magmatic arcs, although some recycled sedimentary and metasedimentary debris is also present.

Research Organization:
Univ. of Arizona, Tucson
OSTI ID:
5361202
Journal Information:
Am. Assoc. Pet. Geol., Bull.; (United States), Journal Name: Am. Assoc. Pet. Geol., Bull.; (United States) Vol. 66:2; ISSN AAPGB
Country of Publication:
United States
Language:
English