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