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Tremolite from
Hengl quarry, Eibenstein an der Thaya, Raabs an der Thaya, Waidhofen an der Thaya District, Lower Austria, Austria


Locality type:Quarry
Classification
Species:Tremolite
Formula:◻Ca2Mg5(Si8O22)(OH)2
Confirmation
Validity:Believed Valid
Associated Minerals Based on Photo Data:
Graphite1 photo of Tremolite associated with Graphite at this locality.
Pyrite1 photo of Tremolite associated with Pyrite at this locality.
Data
Mineral Data:Click here to view Tremolite data
Locality Data:Click here to view Hengl quarry, Eibenstein an der Thaya, Raabs an der Thaya, Waidhofen an der Thaya District, Lower Austria, Austria
Photo GalleryView Gallery (2 photos)
Data Identifiers
Mindat Occurrence Record ID:400750
Long-form Identifier:1:3:400750:0
GUID (UUID V4):e9bb7624-77d9-45b4-9f6a-86782adad288
Nearest other occurrences of Tremolite
0.9km (0.6 miles) Liest quarry, Eibenstein an der Thaya, Raabs an der Thaya, Waidhofen an der Thaya District, Lower Austria, Austria
1.7km (1.1 miles) Kobergraben, Primmersdorf, Raabs an der Thaya, Waidhofen an der Thaya District, Lower Austria, Austria
3.7km (2.3 miles) Zissersdorf, Drosendorf-Zissersdorf, Horn District, Lower Austria, Austria
4.6km (2.9 miles) Unterthürnau, Drosendorf-Zissersdorf, Horn District, Lower Austria, Austria
8.2km (5.1 miles) Chalcedony occurrence, Langau, Horn District, Lower Austria, Austria
17.1km (10.7 miles) Marble quarry, Atzelsdorf, Brunn an der Wild, Horn District, Lower Austria, Austria
21.4km (13.3 miles) Graphite mine, Röhrenbach, Horn District, Lower Austria, Austria
21.8km (13.5 miles) Marble quarries (incl. Renz Quarry; Bundesheer Quarry), Winkl, Röhrenbach, Horn District, Lower Austria, Austria
27.7km (17.2 miles) Töppenitzgraben (Töpenitzgraben; Töbernitzgraben; Töppenitzbach), Altpölla, Pölla, Zwettl District, Lower Austria, Austria
36.9km (23.0 miles) Dörrmühle (Hofmühle), Rastbach, Gföhl, Krems-Land District, Lower Austria, Austria
References
Reference Search (possible matching items)
Journal (article/letter/editorial)
Dome belongs to the Central Sudetes, interpreted as an accretionary wedge, which is located between the...examined in this study as an example of carbonate wall-rock, is from the abandoned quarry in this area. In addition...intruded the metasediments in the form of a vein, or an already-serpentinized peridotite, which was in the...few hundred meters away, and marble from an abandoned quarry in the Kleśnica valley. Both newly collected...synthetic standards were used. Minerals with a lower stability under the electron beam (serpentine, carbonate
Book
in subsurface, undetected by geophysical methods. An updated synthesis of the Roraima Problem, using new...spanning extreme tropical to glacial. • Gansser was an exceptional draftsman, known by his stylish sketches...Publications Related to Northwestern South America 1938 – Der Nevado del Cocuy: Columbianisches Bergerlebnis (selfpublished)...1955 – Ein Beitrag zur Geologie und Petrographie der Sierra Nevada de Santa Marta (Kolumbien, Südamarika)...Mitteilungen aus dem Geologischen Institut der Eidg. Techn. Hochschule und der Universität Zürich, Serie B, Nr.
Report (volume)
resources and tectonics of the Himalayan region, but also an integrated and comprehensive evaluation and consolidation...evolution and metallogeny of the Himalayan region is not an easy task. The task of preparation of such a monograph...68 Uranium mineralisation in Khasa area, Simla district, H . P. 68 Uranium mineralisation around Bh...1.2 in Tehri district, Uttaranchal 71 Ttn-Tungsten mineralisation in Kinnaur district, Himachal Pradesh...Chamoli district, Uttaranchal 75 Sediment hosted base metal mineralisation in Kulu district, Himachal
Journal (article/letter/editorial)
of the metallic phases from the AS#051 ureilite in an attempt to contribute to the understanding of their...some complexities. For example, L chondrites do show an overall increase in metal grain size up to type 5...observe an abrupt change in the cumulative volume fraction curve between S2 and S3 samples, and an increase...hint that a new fraction of coarse grains appears. An observed shift towards larger grain sizes between...linear size-fraction correlation in L5 samples of lower shock stages. We infer that the effects may be constrained
 
Mineral and/or Locality  
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