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Rattlesnake Hills greenstone belt
The Rattlesnake Hills greenstone belt represents a fragment of a partially exposed synformal Archean greenstone belt within the Wyoming craton that was intruded by Cenozoic alkalic volcanics. The supracrustal belt has been subjected to multiphase deformation during the Archean and later brittle deformation during the Laramide orogeny. Ductile deformation during the Archean produced foliation, and at least three episodes of folding.
==Folding==
The exposed core of the Rattlesnake Hills forms an Archean supracrustal belt of metasedimentary and metavolcanic rock that has been intruded by more than 40 Cenozoic alkalic plugs and dikes. Mapping by Hausel〔Hausel, W.D., 1996, Geology and mineralization of the Rattlesnake Hill, Granite Mountains, Wyoming. Wyoming Geological Survey Report of Investigations, 52., 28 p.〕 indicated that the supracrustal belt consisted of a refolded, isoclinally folded, greenstone belt fragment with a lower(?) metasedimentary unit of metapelite, quartzite, banded iron formation and amphibolite named the Barlow Springs Formation. The Barlow Springs Formation is overlain by pillowed metatholeiites of the McDougal Gulch Metavolcanics, which, in turn, is overlain by metagreywacke with intercalated metacherts of the UT Creek Formation. The northern limb of the Rattlesnake synform was not uplifted and presumably underlies the Phanerozoic sediments north of the uplift.
抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』
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