The Blue Mountains: The Ochocos The Wallowas (The Strawberries)...
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1 The Blue Mountains: The Ochocos The Wallowas (The Strawberries)... 46
2 Dorsey & LaMaskin
3 The Wallowa Mountains: Four Plutons Ma 4 48
4 Hell s Canyon: Columbia River Basalt Group unconformably above Mesozoic. 5 49
5 6 50
6 Seven Devils Mountains, ID 7 51
7 Canyon Mountain Complex, south of John Day, OR Alternating peridotite (red) and gabbro layers 13 52
8 11 53
9 Cement Plant near Huntington, OR Martin Bridge Limestone was feedstock until plant closed due to mercury emissions. 8 54
10 U Triassici Fields Creek Formation: sedimentary melange 19 55
11 U Triassici Fields Creek Formation: sedimentary melange 20 56
12 10 57
13 U Triassic Vester Formation: sedimentary melange 17 58
14 18 59
15 12 60
16 Lower Jurassic Suplee Forma<on: marine clas<c rocks 21 with submarine volcanic flows 61
17 22 62
18 M Jurassic Snowshoe Forma<on 23 63
19 146 Ma Dixie Creek Pluton 26 64
20 25 65
21 What Data Do We Use? Paleontology Lithology and Stra<graphy Structural Field Data Radiometric Age Da<ng Paleomagma<sm 66
22 Paleomagnetism of Permian Wallowa Terrane Harbert et al
23 Some images showing plate movements on a sphere hrp://magician.ucsd.edu/essen<als/webbookch16.html#webbookse101.html 68
24 Some images showing plate movements on a sphere hrp://magician.ucsd.edu/essen<als/webbookch16.html#webbookse101.html 69
25 Some images showing plate movements on a sphere hrp://magician.ucsd.edu/essen<als/webbookch16.html#webbookse101.html 70
26 71
27 72
28 Sometime in the geological past Magnetic Declination Magnetic Inclination
29 Plate tectonics moves the plate from (1) to (2) Magnetic Declination Paleo-Magnetic Inclination
30 NB difference in magnetic declinations Magnetic Declination Paleo-Magnetic Inclination 1 2 Modern Declination at (2)
31 But there are problems: 76
32 But there are problems: Tectonic deformation will change the measured paleo-inclination. Here faulting leads us to infer the faulted blocks were deposited at a southern paleo-location, where inclinations are not as steep. 77
33 There are problems Differential compaction of sediments leads to change in measured paleo-inclination in the overlying beds. 78
34 Regional geology Hell s Canyon sites Harbert et al
35 Open square: Paleo-pole this study nb error circle 1=135MA, 2=131MA, 3-7=OTHER POLES Inverted triangle=blue Mt L Jur-E Cret pole Harbert et al
36 Harbert et al
37 Permian Paleo-pole and Hell s Canyon Permian paleopoles: this study suggests Wallowa Terrane formed to NORTH of its present location. Harbert et al
38 Cretaceous Tectonics of the Ochoco Basin: Paleomagnetism Housen and Dorsey
39 Pre-Tertiary geology: nb. Columbia Embayment 84 Housen and Dorsey 2005
40 85 Housen and Dorsey 2005
41 a. Paleomagnetic poles MI=this study, yellow=insular Terranes blue=intermontane terranes b. Mid-Cretaceous Paleo-geography, with paleo-pole, Post-Cretaceous Northward movement of terranes 86 Housen and Dorsey 2005
42 a. Paleomagnetic poles M=this study, yellow=insular Terranes blue=intermontane terranes b. Mid-Cretaceous Paleo-geography, with paleo-pole, Post-Cretaceous Northward movement of terranes These data suggest the Blue Mountains have moved NORTh /- 460 km, and Rotated 37 +/- 7.3 since 93 Ma 87 Housen and Dorsey 2005
43 Basinal response to Triassic-Jurassic Collisional Tectonics in the Blue Mountains Province, Northeastern Oregon Dorsey and LaMaskin
44 89
45 90
46 91
47 92
48 93
49 94
50 95
51 96
52 97
53 98
54 LaMaskin et al
55 LaMaskin et al
56 67 LaMaskin et al
57 Data used in terrane analysis Stra<graphy Paleontology Geochemistry Igneous rock correla<ons Age da<ng Structural rela<ons Paleomagne<sm 102
58 Mesozoic Subduc<on on the Cordilleran Margin Western Sierras Klamaths Blue Mountains 103
59 What is the rela<onship between the Blue Mountain and Klamath Provinces? Dickinson
60 Dickinson
61 Dickinson
62 Dickinson
63 Dickinson
64 Dickinson
65 Dickinson
66 Dickinson
67 Dickinson
68 113
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