| Locality type: | Outcrop |
| Classification |
|---|
|
| Species: | 'Plagioclase' (not an IMA approved species) |
| Formula: | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Confirmation |
|---|
|
| Validity: | Believed Valid |
| Data |
|---|
|
| Mineral Data: | Click here to view Plagioclase data |
| Locality Data: | Click here to view Isdal, Bergenhus, Bergen, Vestland, Norway |
| Data Identifiers |
|---|
|
| Mindat Occurrence Record ID: | 1332666 |
| Long-form Identifier: | 1:3:1332666:1 |
| GUID (UUID V4): | 49083138-6ebf-4e54-856b-3043af1de55a |
| Nearest other occurrences of Plagioclase |
|---|
|
|
| 69.1km (42.9 miles) | ⓘAlsvågen, Bømlo, Vestland, Norway |
| 70.8km (44.0 miles) | ⓘLindøya, Bømlo, Vestland, Norway |
| 91.7km (57.0 miles) | ⓘJordalsnuten Mine, Aurland, Vestland, Norway |
| 97.1km (60.3 miles) | ⓘKrakkanuten pegmatite, Vats, Vindafjord, Rogaland, Norway |
| 97.4km (60.5 miles) | ⓘSøndre Langaneset Quarry, Avløypeneset, Sveio, Vestland, Norway |
| 99.8km (62.0 miles) | ⓘVats Copper Mine, Vats, Vindafjord, Rogaland, Norway |
| References |
|---|
|
|
| Reference Search (possible matching items) |
|---|
 | | Journal (article/letter/editorial) | | published June 19, 2014 Textural Evolution of Plagioclase Feldspar across a Shear Zone: Implications for...OF GEOSCIENCES, UNIVERSITY OF OSLO, N-0316 OSLO, NORWAY RECEIVED AUGUST 16, 2013; ACCEPTED MAY 20, 2014...2014 deformation; EBSD; microtexture; plagioclase; shear Caledonian amphibolite-facies shear zones developed...anorthosites and anorthositic gabbros of the Bergen Arcs, western Norway, allow a detailed study of the relationships...progressive development of microstructure in the plagioclase feldspars, leading up to their deformation in |  | | Journal (article/letter/editorial) | | Perspectives Metamorphic Processes and Seismicity: the Bergen Arcs as a Natural Laboratory Andrew Putnis1,2*...Geosciences, University of Oslo, Blindern, N-0316 Oslo, Norway *Corresponding author. Telephone: þ61 0466 339...E-mail: Andrew.putnis@ curtin.edu.au ABSTRACT In the Bergen Arcs rocks that formed the root zone of the Caledonian...understanding metamorphism in terranes such as the Bergen Arcs could be made by greater attention to the...relationship between seismicity and metamorphism. The Bergen Arcs provide a natural laboratory in which it should |
|
