New occurrence of wulfenite at the Stari Trg-Trepča ore deposit
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Metapodaci
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Wulfenite (PbMoO4) is a rather rare mineral, and according to that, every new occurrence deserves considerable attention. This mineral was discovered at the Stari Trg-Trepča ore deposit in the paragenesis with galena, sphalerite, pyrite, calcite and rhodochrosite. It appears together with calcite at the calcite crust formed over pyrite zone, as honey-yellow crystals of pyramidal shapes, with size of 5-25 mm. The X-ray powder diffraction pattern, as well as calculated crystallographic parameters in the adequate tetragonal I41/a space group of: a = 5,428(2) Å; c = 12,111(4) Å; and V = 356,8(2) Å3; are in very good agreement with the literature data. Wulfenite most probably originated as secondary mineral from cerussite at the oxidation zone.
Ključne reči:
Stari Trg-Trepča / wulfenite / new occurrence / X-ray investigationsIzvor:
Proceedings - 15th Congress of Geologists of Serbia with international participation, 2010, 45-45Izdavač:
- Belgrade : Serbian Geological Society
Institucija/grupa
IHTMTY - CONF AU - Tančić, Pavle AU - Tomić, Zorica PY - 2010 UR - https://cer.ihtm.bg.ac.rs/handle/123456789/6039 AB - Wulfenite (PbMoO4) is a rather rare mineral, and according to that, every new occurrence deserves considerable attention. This mineral was discovered at the Stari Trg-Trepča ore deposit in the paragenesis with galena, sphalerite, pyrite, calcite and rhodochrosite. It appears together with calcite at the calcite crust formed over pyrite zone, as honey-yellow crystals of pyramidal shapes, with size of 5-25 mm. The X-ray powder diffraction pattern, as well as calculated crystallographic parameters in the adequate tetragonal I41/a space group of: a = 5,428(2) Å; c = 12,111(4) Å; and V = 356,8(2) Å3; are in very good agreement with the literature data. Wulfenite most probably originated as secondary mineral from cerussite at the oxidation zone. PB - Belgrade : Serbian Geological Society C3 - Proceedings - 15th Congress of Geologists of Serbia with international participation T1 - New occurrence of wulfenite at the Stari Trg-Trepča ore deposit SP - 45 EP - 45 UR - https://hdl.handle.net/21.15107/rcub_cer_6039 ER -
@conference{ author = "Tančić, Pavle and Tomić, Zorica", year = "2010", abstract = "Wulfenite (PbMoO4) is a rather rare mineral, and according to that, every new occurrence deserves considerable attention. This mineral was discovered at the Stari Trg-Trepča ore deposit in the paragenesis with galena, sphalerite, pyrite, calcite and rhodochrosite. It appears together with calcite at the calcite crust formed over pyrite zone, as honey-yellow crystals of pyramidal shapes, with size of 5-25 mm. The X-ray powder diffraction pattern, as well as calculated crystallographic parameters in the adequate tetragonal I41/a space group of: a = 5,428(2) Å; c = 12,111(4) Å; and V = 356,8(2) Å3; are in very good agreement with the literature data. Wulfenite most probably originated as secondary mineral from cerussite at the oxidation zone.", publisher = "Belgrade : Serbian Geological Society", journal = "Proceedings - 15th Congress of Geologists of Serbia with international participation", title = "New occurrence of wulfenite at the Stari Trg-Trepča ore deposit", pages = "45-45", url = "https://hdl.handle.net/21.15107/rcub_cer_6039" }
Tančić, P.,& Tomić, Z.. (2010). New occurrence of wulfenite at the Stari Trg-Trepča ore deposit. in Proceedings - 15th Congress of Geologists of Serbia with international participation Belgrade : Serbian Geological Society., 45-45. https://hdl.handle.net/21.15107/rcub_cer_6039
Tančić P, Tomić Z. New occurrence of wulfenite at the Stari Trg-Trepča ore deposit. in Proceedings - 15th Congress of Geologists of Serbia with international participation. 2010;:45-45. https://hdl.handle.net/21.15107/rcub_cer_6039 .
Tančić, Pavle, Tomić, Zorica, "New occurrence of wulfenite at the Stari Trg-Trepča ore deposit" in Proceedings - 15th Congress of Geologists of Serbia with international participation (2010):45-45, https://hdl.handle.net/21.15107/rcub_cer_6039 .