Rocky Mountain (63rd Annual) and Cordilleran (107th Annual) Joint Meeting (18–20 May 2011)

Paper No. 1
Presentation Time: 8:05 AM

U-PB ZIRCON GEOCHRONOLOGY AND HF ISOTOPE GEOCHEMISTRY OF THE MOUNTAIN HOME METAMORPHIC COMPLEX, BLUE MOUNTAINS PROVINCE, NORTHEASTERN OREGON


ANDERSON, Bryan Scott1, SCHWARTZ, Joshua J.1, JOHNSON, Kenneth2, WOODEN, Joseph L.3 and MUELLER, Paul A.4, (1)Department of Geological Sciences, University of Alabama, Box 870338, Tuscaloosa, AL 35487, (2)Department of Natural Sciences, University of Houston-Downtown, 1 Main Street, Suite N813, Houston, TX 77002, (3)USGS-Stanford Ion Microprobe Laboratory, Stanford University, Stanford, CA 94305, (4)Department of Geological Sciences, University of Florida, 241 Williamson Hall, Gainesville, FL 32611-2120, bsanderson@crimson.ua.edu

Orogenesis in the Blue Mountains Province (BMP) of NE Oregon involved the accretion of various tectonostratigraphic terranes in concert with syn-tectonic magmatism. Timescales of deformation, metamorphism and magmatism in this region of the Cordillera are poorly constrained, hindering detailed understanding of the timing of tectonic events and the magmatic and metamorphic processes accompanying them. In the Mountain Home Metamorphic Complex (MHMC), an enigmatic sequence of medium-grade metavolcanic and metasedimentary rocks is intruded by two groups of variably deformed plutons. Metamorphic rocks include chlorite+biotite+garnet±sillimanite±staurolite schist, and keratophyre and metatuff which grade into chlorite schist near fault contacts. This degree of metamorphism is uncommon in the BMP, and contrasts with adjacent rocks in the Baker and Wallowa terranes.

Two distinct plutonic suites intrude metamorphic host rocks: 1) deformed hornblende tonalite and trondhjemite (Group 1), and 2) undeformed biotite-hornblende tonalite, biotite-hornblende quartz diorite, and hornblende gabbronorite (Group 2). Quartz microstructures in deformed plutons display evidence for grain-boundary migration and subgrain-rotation recrystallization, features which are absent in Group 2 plutons. 206Pb/238U zircon ages for Group 1 plutons range from 161.3 to 149.5 Ma; whereas Group 2 plutons yield ages ranging from 147.8 Ma to 145.5 Ma. These ages bracket deformation to between 149.5 to 147.9 Ma, which contrasts with the timing of previously documented tectonic events in the BMP. Initial εHf values range from +16.3 to +10.2 in Group 1 plutons and +13.8 to +4.2 in Group 2 plutons. These values overlap and extend to lower values than average modern island arc crust. Based on the new deformational period and degree of metamorphism in the MHMC we suggest that it may be a new terrane in the BMP.

Unit

206Pb/238U age

error

εHfi

(Ma)

(2σ)

(range)

Group 1: Deformed

Metatrondhjemite of Pearson Creek

161.3

1.2

n.d.

Metatonalite of California Gulch

152.7

1.2

16.3-10.2

Trondhjemite of Johnson creek

149.5

1.7

13.9-10.5

Group 2: Undeformed

Quartz diorite of Alexander Creek

147.9

2.4

13.8-8.3

Gabbronorite of Carney Butte

147.8

1.6

12.8-5.8

Tonalite of Granite Meadows

146.5

1.2

11.5-7.2

Gabbronorite of Ridenor Canyon

145.6

0.5

10.7-4.2