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Title: Isotopic evidence for the origin of mesozoic and cenozoic granitic plutons in the northern Great Basin

Journal Article · · Geology; (USA)
;  [1]
  1. California Institute of Technology, Pasadena (USA)

{sup 18}O/{sup 16} ratios of granitic rocks in western North America reflect source-rock lithologies, providing insight into the geology of the deep continental crust. In a 400-km-wide, 800-km-long, east-west transect through the northern Great Basin, the Mesozoic and Cenozoic plutons define three zones: western low {sub 18}O zone (WZ), {delta}{sup 18}O = +6 to +8.5; central high -{sup 18}O zone (CZ), {delta}{sup 18}O = +9 to +13; eastern zone (EZ) (Utah), {delta}{sup 18}O = +7 to +9. The WZ-CZ boundary is analogous to the {delta}{sup 18}O step in the Peninsular Ranges batholith (PRB). A similarly abrupt ({sup 87}Sr/{sup 86}Sr){sub i} step (<0.708 to the west and >0.710 to the east) defined by Farmer and DePaolo (1983) lies 150-200km east of the WZ-CZ {sup 18}O/{sup 16}O step, dividing the CZ into two subzones: V-type in the west, corresponding to the eastern half of the PRB (but much wider due to regional Cenozoic extension); and S-type to the east. A plausible source for the high-{sup 87}Sr, low-{epsilon}{sub Nd}, S-type subzone is a late Precambrian (miogeoclinal) metasedimentary section, whereas the V-type source appears to be a Phanerozoic volcanogenic (eugeoclinal) accreted terrane. Both source regions have very high {delta}{sup 18}O (+9 to +16) but radically different {sup 87}Sr/{sup 86}Sr (and {epsilon}{sub Nd}); thus, the authors would not place the buried edge of the > 1.5 Ga craton beneath the {sup 87}Sr/{sup 86}Sr step, but farther east near the EZ boundary. The authors instead that this step is a sharp lithologic and age boundary (a suture-zone ) within the giant prism of sediments and volcanics in Nevada.

OSTI ID:
7254097
Journal Information:
Geology; (USA), Vol. 17:7; ISSN 0091-7613
Country of Publication:
United States
Language:
English