Composition of modern stream sand in a humid climate derived from a low-grade metamorphic and sedimentary foreland fore-thrust belt of North Georgia

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Authors:Mack, Greg H.
Author Affiliations:Primary:
N.M. State Univ., Dep. Earth Sci., Las Cruces, NM, United States
Volume Title:Journal of Sedimentary Petrology
Source:Journal of Sedimentary Petrology, 51(4), p.1247-1258. Publisher: Society of Economic Paleontologists and Mineralogists, Tulsa, OK, United States. ISSN: 0022-4472
Publication Date:1981
Note:In English. 21 refs.; illus. incl. 1 table, geol. sketch map
Summary:Conditions of tectonics and drainage in north-central Georgia provide an excellent natural laboratory to study the composition of stream sand derived from a low-grade metamorphic and sedimentary foreland fold-thurst belt under humid climatic conditions. The streams head in a high-relief phyllite, schist, and metasandstone terrain and flow westward across a bounding fault into lower relief Paleozoic shales, cherty carbonates, and quartz arenites. The relative abundance of the source rock types in the drainage basin of each sample site was determined and a "source rock ratio" was calculated as the ratio of the area underlain by metamorphic rock to the total area of the drainage basin. Low-grade metamorphic source rocks supply subequal amounts of monocrystalline quartz, polycrystalline quartz. and foliated quartz-mica rock fragments to stream sediment, whereas sand from the sedimentary source terrain consists primarily of monocrystalline quartz, a surprisingly large number of pelitic rock fragments, and chert. Mixing of sediment from both source rock types is recognizable on the quartz provenance diagram of Young (1976) by a high instability index (unstable polycrystalline quartz/total polycrystalline quartz) and a low polycrystallinity index (polycrystalline/total quartz). This diagram is especially sensitive to the presence of sandstones as source rocks, which further decreases the polycrystallinity index. The ratio of metamorphic rock fragments to total rock fragments also is directly related to the source rock ratio. Modern sand derived from the foreland fold-thurst belt of north Georgia can be distinguished from Neogene subduction complex-derived sand and collision orogen-derived sand on QFL, LmLsLv, and QpLsmLvm provenance diagrams by containing less total feldspar, more total quartz, and no volcanic rock fragments. The concepts developed from the recent sand are applied to the Mississippian Parkwood Formation, Alabama, and the Cretaceous Muddy Formation, Montana. The results suggest that both sandstone units were derived from foreland fold-thrust belts but that the Parkwood source area contained a greater proportion of low-grade metamorphic source rocks than the source area of the Muddy. [H.R.B.]
Subjects:Clastic sediments; Composition; Fluvial environment; Fluvial sedimentation; Humid environment; Low-grade metamorphism; Metamorphic rocks; Metamorphism; Orogenic belts; Provenance; Sand; Sedimentary petrology; Sedimentary rocks; Sedimentation; Sediments; Terrestrial environment; Appalachians; Bartow County Georgia; Blue Ridge Province; Cherokee County Georgia; Fannin County Georgia; Georgia; Gilmer County Georgia; Gordon County Georgia; Murray County Georgia; North America; Pickens County Georgia; United States; Valley and Ridge Province
Coordinates:N340000 N350000 W0841500 W0850000
Abstract Numbers:82M/5012
Record ID:1982032750
Copyright Information:GeoRef, Copyright 2019 American Geosciences Institute.
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