Classification |
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Species: | Titanite |
Formula: | CaTi(SiO4)O |
Confirmation |
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Validity: | Believed Valid |
Data |
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Mineral Data: | Click here to view Titanite data |
Locality Data: | Click here to view Lopuchowo, Suwałki Massif, Suwałki County, Podlaskie Voivodeship, Poland |
Data Identifiers |
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Mindat Occurrence Record ID: | 898804 |
Long-form Identifier: | 1:3:898804:1 |
GUID (UUID V4): | 6c5a8b8e-ba88-45fb-bb09-a65a2377b330 |
Nearest other occurrences of Titanite |
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7.3km (4.6 miles) | ⓘPawłówka PIG-1 borehole, Nowa Pawłówka, Gmina Przerośl, Suwałki County, Podlaskie Voivodeship, Poland |
17.4km (10.8 miles) | ⓘFilipów IG-1 borehole, Wólka, Gmina Bakałarzewo, Suwałki County, Podlaskie Voivodeship, Poland |
29.1km (18.1 miles) | ⓘKrasnopol PIG-6 borehole, Krasnopol, Gmina Krasnopol, Sejny County, Podlaskie Voivodeship, Poland |
66.1km (41.1 miles) | ⓘTajno alkaline-carbonatite massif, Podlaskie Voivodeship, Poland |
References |
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Reference Search (possible matching items) |
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| | Report (issue) | complex of the 830 km2 Chepovichi gabbro-anorthosite massif. The ore body has an irregular oval shape (2.3...Volodarsk-Volynsk gabbro-anorthosite massif within the Korosten pluton. The area of the massif is 1250 km2. The ore body...the southern part of the Smela gabbro-anorthosite massif. The deposit is lens-shaped, with an overall length...aulacogen, separating the USH from the Voronezh massif in Russia. The Late Palaeozoic volcano-plutonic...Precambrian basement and form the Pokrovo-Kireyevo massif, whereas the second is distributed throughout the | | | Report (edition) | complex of the 830 km2 Chepovichi gabbro-anorthosite massif. The ore body has an irregular oval shape (2.3...Volodarsk-Volynsk gabbro-anorthosite massif within the Korosten pluton. The area of the massif is 1250 km2. The ore body...the southern part of the Smela gabbro-anorthosite massif. The deposit is lens-shaped, with an overall length...aulacogen, separating the USH from the Voronezh massif in Russia. The Late Palaeozoic volcano-plutonic...Precambrian basement and form the Pokrovo-Kireyevo massif, whereas the second is distributed throughout the |
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