| Classification |
|---|
|
| Species: | 'Monazite' (not an IMA approved species) |
| Formula: | REE(PO4) |
| Confirmation |
|---|
|
| Validity: | Believed Valid |
| Data |
|---|
|
| Mineral Data: | Click here to view Monazite data |
| Locality Data: | Click here to view Zishineni, Sinceni West area, Sinceni Mtn, Lubombo Region, Eswatini |
| Data Identifiers |
|---|
|
| Mindat Occurrence Record ID: | 1350543 |
| Long-form Identifier: | 1:3:1350543:5 |
| GUID (UUID V4): | e9f1ed22-79c3-40cb-b7cf-8f6bf63ad68b |
| References |
|---|
|
Grew, E.S., Bosi, F., Ros, L., Kristiansson, P., Gunter, M.E., HĂĄlenius, U., Trumbull, R.B., Yates, M.G. (2018): Fluor-elbaite, lepidolite and Ta-Nb oxides from a pegmatite of the 3000 Ma Sinceni Pluton, Swaziland: evidence for lithium-cesium-tantalum (LCT) pegmatites in the Mesoarchean. European Journal of Mineralogy 30, 205-218. |
| Reference Search (possible matching items) |
|---|
 | Grew, Edward S., Bosi, Ferdinando, Ros, Linus, Kristiansson, Per, Gunter, Mickey E., Hålenius, Ulf, Trumbull, Robert B., Yates, Martin G. (2018) Fluor-elbaite, lepidolite and Ta–Nb oxides from a pegmatite of the 3000 Ma Sinceni Pluton, Swaziland: evidence for lithium–cesium–tantalum (LCT) pegmatites in the Mesoarchean. European Journal of Mineralogy, 30 (2) 205-218 doi:10.1127/ejm/2017/0029-2686 | Journal (article/letter/editorial) | | and Ta–Nb oxides from a pegmatite of the 3000 Ma Sinceni Pluton, Swaziland: evidence for lithium–cesium–tantalum...assemblage from a pegmatite near Zishineni associated with the ca. 3000 Ma Sinceni Pluton presents unusual interest...Sps93Alm4Grs3) in scattered grains up to 0.5 mm across and monazite. Oxides occur sparsely in muscovite, rarely in...± 4 Ma evaporation Pb–Pb ages reported for the Sinceni Pluton and Rb/Sr mineral ages ranging from 2906...lithium–cesium–tantalum (LCT) family of pegmatites. The Sinceni magma is most plausibly derived from a metasedimentary |  | | Journal (article/letter/editorial) | | Archean fertile granite-pegmatite system: the Sinceni Pluton in Swaziland Robert B. Trumbull Lehrstuhl...granite-pegmatite system: the Sinceni Pluton in Swaziland. Precambrian Res., 61: 89-116. The Sinceni Pluton in the eastern...and muscovite Rb-Sr ages of 3000+ 100 Ma. The Sinceni Pluton is asymetrically zoned in chemical and mineralogical...mineralogical composition, and the Sinceni pegmatite field occurs at the most differentiated southern...unlikely to constitute a direct source of the Sinceni Pluton according to the Sr isotopic and age data |
|
