Locality type: | Quarry |
Classification |
---|
|
Species: | Titanite |
Formula: | CaTi(SiO4)O |
Confirmation |
---|
|
Validity: | Believed Valid |
Associated Minerals Based on Photo Data: |
---|
|
Albite | ⓘ1 photo of Titanite associated with Albite at this locality. |
Chamosite | ⓘ1 photo of Titanite associated with Chamosite at this locality. |
Data |
---|
|
Mineral Data: | Click here to view Titanite data |
Locality Data: | Click here to view Paszowice quarry, Gmina Paszowice, Jawor County, Lower Silesian Voivodeship, Poland |
Data Identifiers |
---|
|
Mindat Occurrence Record ID: | 427914 |
Long-form Identifier: | 1:3:427914:3 |
GUID (UUID V4): | fede8d69-480f-47f2-b32e-0b74d4387173 |
Nearest other occurrences of Titanite |
---|
|
|
7.7km (4.8 miles) | ⓘChełmiec mine, Chełmiec, Gmina Męcinka, Jawor County, Lower Silesian Voivodeship, Poland |
10.4km (6.5 miles) | ⓘGrabina I quarry, Strzegom, Gmina Strzegom, Świdnica County, Lower Silesian Voivodeship, Poland |
11.8km (7.3 miles) | ⓘGrabina, Strzegom, Gmina Strzegom, Świdnica County, Lower Silesian Voivodeship, Poland |
14.7km (9.1 miles) | ⓘPillow lavas quarry, Sichów, Gmina Męcinka, Jawor County, Lower Silesian Voivodeship, Poland |
25.7km (16.0 miles) | ⓘHoffnung Mine, Colourful Lakelets, Wieściszowice, Gmina Marciszów, Kamienna Góra County, Lower Silesian Voivodeship, Poland |
25.8km (16.0 miles) | ⓘAmphibolite quarry, Wieściszowice, Gmina Marciszów, Kamienna Góra County, Lower Silesian Voivodeship, Poland |
27.5km (17.1 miles) | ⓘDzicza Góra, Rędziny, Gmina Kamienna Góra, Kamienna Góra County, Lower Silesian Voivodeship, Poland |
27.7km (17.2 miles) | ⓘBorówno melaphyre quarry, Krzeszów, Gmina Kamienna Góra, Kamienna Góra County, Lower Silesian Voivodeship, Poland |
28.1km (17.5 miles) | ⓘOwiecznik melaphyre quarry, Boguszów-Gorce, Wałbrzych County, Lower Silesian Voivodeship, Poland |
28.6km (17.8 miles) | ⓘGołaszyce granite quarry, Gmina Marcinowice, Świdnica County, Lower Silesian Voivodeship, Poland |
References |
---|
|
|
Reference Search (possible matching items) |
---|
| | Journal (article/letter/editorial) | Karkonosze Massif and Its Eastern Metamorphic Cover (SW Poland) Stanisław Z. Mikulski 1, * , Ian S. Williams 2...Research Institute, Rakowiecka 4, 00-975 Warszawa, Poland Research School of Earth Sciences, Australian National...University, Żwirki i Wigury 93, 02-089 Warszawa, Poland; Jan.Wierchowiec@uw.edu.pl Correspondence: stanislaw...SW edge of the East-European Platform (Figure 1, lower inset). The KP is surrounded by variably metamorphosed...Abbreviations: MO—Moldanubian Zone, MS—Moravo-Silesian Zone, show the area of the main map. Abbreviations: | | | Journal (article/letter/editorial) | subdivided into two units (the Lower Unit and the Upper Unit). Orthogneisses of the Lower Unit are mostly banded...Earth Sciences, University of Silesia, Sosnowiec, Poland e-mail: jolanta.burda@us.edu.pl U. Klötzli Department...massif (Fig. 1) is subdivided into two units, the Lower Unit and the Upper Unit, both with different lithologies...(Kohút and Janak 1994; Gawęda et al. 1998). The Lower Unit consists of mica schists, gneisses and minor...typical microfabrics of orthogneisses from the Lower Unit (sample OZ1); b, c augen-banded structures | | | Journal (article/letter/editorial) | 2006; Tomkins et al. 2007) and ±20 °C for Zr-in-titanite (Hayden et al. 2008), similar to the measured...reflect a different P-T condition (either higher or lower than the average), and calculated an average mica...than positive ∆S; these terms may be balanced by a lower ∆V. The steep slopes and close spacing of lnK isopleths...highest temperatures. We ascribe this misfit to lower a(rt) in these rocks. Thus, both models can be reconciled...higher Mg/(Fe+Mg) tends toward lower Ti in many rocks, but also toward lower Al and higher silicon. Given | | | Book | (KOKOTSKO) STOCK ……………………………………………………………... 76 1.22. LOWER VLTAVA COMPOSITE MASSIF …………………………………………………… 77...intrusions of the CBCB single-zircon dating indicates Lower Carboniferous (Tournaisian–Viséan) ages and their... Geological environment: Neoproterozoic up to Lower Devonian pellites, greywackes, metabasalts, keratophyres...strata and the Blatná Granodiorite intrudes the Lower Devonian sediments. Xenoliths of coarse-grained...(Kodymová and Vejnar 1974) 1 – titanite-ilmenite (basic rocks), 2 – titanite-orthite-ilmenite (types Čertovo |
|
Paszowice quarry, Gmina Paszowice, Jawor County, Lower Silesian Voivodeship, Poland