| ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
Journal of Petrology Volume 42 Number 5 Pages 901-929 2001
© Oxford University Press 2001
Petrology and Geochemistry of the Late Eocene Harrison Pass Pluton, Ruby Mountains Core Complex, Northeastern Nevada
1DEPARTMENT OF GEOSCIENCES, TEXAS TECH UNIVERSITY, LUBBOCK, TX 79409-1053, USA
2DEPARTMENT OF GEOLOGY AND GEOPHYSICS, UNIVERSITY OF WYOMING, LARAMIE, WY 82071-3006, USA
3DEPARTMENT OF GEOLOGY, RICE UNIVERSITY, HOUSTON, TX 77251-1892, USA
4DEPARTMENT OF CHEMISTRY AND BIOCHEMISTRY, TEXAS TECH UNIVERSITY, LUBBOCK, TX 79409-1053, USA
The late Eocene Harrison Pass pluton was emplaced in the transition zone between the infrastructure and suprastructure of the Ruby Mountains core complex. Emplacement was at 
3 kbar pressure and was in two stages: early stage tonalitic to monzogranitic magmas, followed by late-stage monzogranites and mafic dikes. The early stage began with emplacement of biotite ± hornblende granodiorite of Toyn Creek, followed by the biotite monzogranite of Corral Creek. Quenched equivalents of these units are preserved as porphyritic dikes in the roof. Leucocratic monzogranite that forms cupolas in the roof zone represents the product of fractional crystallization of the early magmas. Al-in-hornblende barometry and the presence of magmatic epidote suggest that early stage magmas resided at a pressure of 5-6 kbar before emplacement in the upper crust. Compositional variation in the Toyn Creek and Corral Creek units is essentially linear, and can be explained by mixing of a tonalitic end member with a monzogranitic end member such as evolved samples of the monzogranite of Corral Creek. The tonalitic end member was itself a hybrid that formed by interaction of mafic magma with crustal melts. The monzogranitic end member is a crustal melt that escaped hybridization. Nd isotopic compositions of the early stage are heterogeneous and do not correlate with degree of differentiation, which is consistent with a compositionally heterogeneous felsic end member. Elemental variation in the early stage of the pluton is unusual because of its essentially linear trends, which suggest a single mixing event before emplacement in the upper crust. Late-stage activity consisted of three pulses of monzogranitic magma plus sparse mafic dikes. The largest and youngest of these pulses, the two-mica monzogranite of Green Mountain Creek, is distinct from all other units in the presence of restitic enclaves, low 
Nd, and high initial 87Sr/86Sr. Pod-like bodies of leucocratic biotite ± amphibole monzogranite and sheets and dikes of leucocratic two-mica monzogranite make up the other late-stage granites. These rocks display deep negative Eu anomalies and show wide, non-systematic concentrations of high field strength elements; however, their isotopic compositions are identical to those of the early stage rocks. They are thought to be small melt fractions of the lower to middle crust. Their elemental compositions are thought to result from the effects of residual plagioclase and accessory minerals. The variable and non-systematic isotopic compositions of all granitic units in the pluton suggest a heterogeneous source region, such as the Proterozoic Mojave province.
KEY WORDS: granite; mixing; crustal melting; Nevada
CiteULike 
Connotea 
Del.icio.us What's this?
This article has been cited by other articles:
|
|
 |
|
  E. B. Ryskamp, J. T. Abbott, E. H. Christiansen, J. D. Keith, J. D. Vervoort, and D. G. Tingey Age and petrogenesis of volcanic and intrusive rocks in the Sulphur Spring Range, central Nevada: Comparisons with ore-associated Eocene magma systems in the Great Basin Geosphere, June 1, 2008; 4(3): 496 - 519. [Abstract] [Full Text] [PDF]
|
|
|
|
 |
|
 E. Slaby and H. Martin Mafic and Felsic Magma Interaction in Granites: the Hercynian Karkonosze Pluton (Sudetes, Bohemian Massif) J. Petrology, February 1, 2008; 49(2): 353 - 391. [Abstract] [Full Text] [PDF]
|
|
|
|
 |
|
 W. A. Sullivan and A. W. Snoke Comparative anatomy of core-complex development in the northeastern Great Basin, U.S.A. Rocky Mountain Geology, July 1, 2007; 42(1): 1 - 29. [Abstract] [Full Text] [PDF]
|
|
|
|
 |
|
 M. W. Ressel and C. D. Henry Igneous Geology of the Carlin Trend, Nevada: Development of the Eocene Plutonic Complex and Significance for Carlin-Type Gold Deposits Economic Geology, March 1, 2006; 101(2): 347 - 383. [Abstract] [Full Text] [PDF]
|
|
|
|
 |
|
 J.F. DAVIES and R.E. WHITEHEAD Alkali-Alumina and MgO-Alumina Molar Ratios of Altered and Unaltered Rhyolites Exploration and Mining Geology, January 1, 2006; 15(1-2): 75 - 88. [Abstract] [Full Text] [PDF]
|
|
|
|
|
|
O. BACHMANN and G. W. BERGANTZ On the Origin of Crystal-poor Rhyolites: Extracted from Batholithic Crystal Mushes J. Petrology, August 1, 2004; 45(8): 1565 - 1582. [Abstract] [Full Text] [PDF]
|
|
|
|
|
|
K. A. Howard Crustal Structure in the Elko-Carlin Region, Nevada, during Eocene Gold Mineralization: Ruby-East Humboldt Metamorphic Core Complex as a Guide to the Deep Crust Economic Geology, April 1, 2003; 98(2): 249 - 268. [Abstract] [Full Text] [PDF]
|
|
|
|
|
|
S.-Y. LEE, C. G. BARNES, A. W. SNOKE, K. A. HOWARD, and C. D. FROST Petrogenesis of Mesozoic, Peraluminous Granites in the Lamoille Canyon Area, Ruby Mountains, Nevada, USA J. Petrology, April 1, 2003; 44(4): 713 - 732. [Abstract] [Full Text] [PDF]
|
|