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Detrital modes of recent deep‐sea sands and their relation to tectonic setting: a first approximation
Author(s) -
VALLONI RENZO,
MAYNARD J. BARRY
Publication year - 1981
Publication title -
sedimentology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.494
H-Index - 108
eISSN - 1365-3091
pISSN - 0037-0746
DOI - 10.1111/j.1365-3091.1981.tb01664.x
Subject(s) - geology , lithic fragment , tectonics , petrography , diagenesis , back arc basin , tectonic subsidence , continental margin , feldspar , subduction , paleontology , petrology , geomorphology , geochemistry , quartz , sedimentary basin
Complete petrographic analyses of modern deep‐sea sands are surprisingly rare, but are needed if problems such as the influence of tectonics on petrology, or changes in petrology due to diagenesis, are to be understood in ancient sandstones. This paper is a first attempt, using data from our own study of 80 sands plus data from the literature, to establish a baseline for modern deep‐sea sands with which ancient sandstones can be compared. We assigned sands to five plate‐tectonic categories, each of which has a distinct average petrologic composition: (1) basins associated with trailing‐edge continental margins, Q 62 F 26 L 12 ; (2) with leading‐edge continental margins, either subduction, Q 16 F 53 L 31 , or (3) strike‐slip, Q 34 F 39 L 27 ; (4) back‐arc basins, Q 20 F 29 L 51 ; (5) fore‐arc basins, Q 8 F 17 L 75 . The amount and type of lithic fragments and the type of feldspar are particularly important discriminators, the amount of quartz less so. Trailing‐edge and fore‐arc basins have quite distinctive compositions, but back‐arc basins and basins near the two types of leading‐edge margins show some overlap, and thus may be hard to differentiate in ancient sandstones.