Locality type: | Massif |
Classification |
---|
|
Species: | Andradite |
Formula: | Ca3Fe23+(SiO4)3 |
Confirmation |
---|
|
Validity: | Believed Valid |
Data |
---|
|
Mineral Data: | Click here to view Andradite data |
Locality Data: | Click here to view Agardag ultramafic massif, Tes-Khemsky District, Tuva, Russia |
Data Identifiers |
---|
|
Mindat Occurrence Record ID: | 1290332 |
Long-form Identifier: | 1:3:1290332:0 |
GUID (UUID V4): | 6eb65df3-a0f9-49ee-81fb-af38e4283f2c |
References |
---|
|
Palyanova, G. A., Murzin, V. V., Zhuravkova, T. V., & Varlamov, D. A. (2018). Au-Cu-Ag mineralization in rodingites and nephritoids of the Agardag ultramafic massif (southern Tuva, Russia). Russian Geology and Geophysics, 59(3), 238-256. |
Reference Search (possible matching items) |
---|
| | Journal (article/letter/editorial) | of low-temperature Alpine-type serpentinized ultramafic T rocks (Salem et al., 2012; Surour, 2017)...with ~12% H2O (Mével, 2003). Metasomatism of ultramafic rocks AN continues from sea-floor serpentinization...all of the studied areas (Fig. 1), ophiolitic ultramafic rocks are mostly serpentinites that occurs as...ones, are useful for petrogenesis of mafic and ultramafic rocks in opholites. T Both rodingites and unrodingitized...rodingite from the Hafafit area is CE grossular-andradite which can be also seen on the mole% ternary diagram |
|