An ore genetic model for the Lubin—Sieroszowice mining district, Poland

Wodzicki, Antoni; Piestrzyński, Adam

doi:10.1007/bf03326394

Cited by 57 publications

(20 citation statements)

References 42 publications

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“…Wagner and Lorenz, 2002). Although many early studies advocated a syngenetic origin for the mineralization, current opinion supports a post-depositional (diagenetic or epigenetic) origin for the majority of the sulphide mineralization (e.g., Jowett, 1986;Jowett et al, 1987b;Kucha and Pawlikowski, 1986;Cathles et al, 1993;Wodzicki and Piestrzynski, 1994;Blundell et al, 2003;Brown, 2014). Cited evidence includes: (1) textures that show sulphides replacing quartz grains, calcite cement, and pyrite framboids; (2) metal zonation that is locally discordant to the stratigraphy; and (3) the presence of mineralized veinlets.…”

Section: Geological Overviewmentioning

confidence: 99%

A multistage origin for Kupferschiefer mineralization

Alderton

Selby

Kucha

et al. 2016

Ore Geology Reviews

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Section: Geological Overviewmentioning

confidence: 99%

A multistage origin for Kupferschiefer mineralization

Alderton

Selby

Kucha

et al. 2016

Ore Geology Reviews

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“…As com monly ar gued, Rotliegend for ma tion wa ters were char ac ter ized by a rel a tively low pH, high Eh (in the sta bil ity field of he ma tite), con sid er able sa lin ity, high con cen tra tion of chloride ions, and el e vated tem per a tures in creas ing the abil ity of the fluid to trans port met als (e.g., Jowett et al, 1987;Wodzicki and Piestrzyñski, 1994;Oszczepalski, 1999;Speczik et al, 2003). Such flu ids can dis solve as lit tle as up to 4 ppb REE (Gieré, 1996;Jaireth et al, 2014), but chlo ride complexation and REE mo bil ity suf fi ciently in creases with in creas ing tem pera ture (Gam mons et al, 1996;Gieré, 1996;Migdisov et al, 2016).…”

Section: Interpretation and Discussionmentioning

confidence: 99%

Controls on the distribution of rare earth elements in the Kupferschiefer series of SW Poland

Oszczepalski¹,

Chmielewski²,

Mikulski³

2016

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1 Pol ish Geo log i cal In sti tute -Na tional Re search In sti tute, Rakowiecka 4, 00-975 Warszawa, Po land Oszczepalski, S., Chmielewski, A., Mikulski, S.Z., 2016. Con trols on the dis tri bu tion of rare earth el e ments in the Kupferschiefer se ries of SW Po land. Geo log i cal Quar terly, 60 (4): 811-826, doi: 10.7306/gq.1325 This study deals with the spa tial dis tri bu tion and the PAAS-nor mal ized pat terns of rare earth el e ments (REE) stud ied by ICP-MS in the Kupferschiefer se ries of SW Po land. The most char ac ter is tic fea ture is a pro gres sive en rich ment in REE content (in clud ing Y and Sc) out ward from the rocks with py ritic and Pb-Zn min er al isa tion, across the rocks with cop per min er alisa tion, to wards the ox i dized (Rote Fäule) ar eas. The same trend can also be ob served with re spect to LREE, MREE and HREE. Whereas REE dis tri bu tion di a grams for shales with py rite and Pb-Zn min er al isa tion are al most flat, di a grams for shales with he ma tite and cop per min er al isa tion are con vex-up ward and the stron gest con vex ity is at trib uted to the tran si tion from hematitic al ter ation to cop per-rich rocks. REE dis tri bu tion di a grams nor mal ized to PAAS show strong MREE en richment rel a tive to LREE and HREE, which is typ i cally the high est in the he ma tite zone, lower in shale with cop per min er al isation, and the low est in shales with Pb-Zn and py rite min er al isa tion. The sys tem atic in crease in the con cen tra tion of REE to wards the Rote Fäule, and the strong en rich ment in MREE in the tran si tion zone are in dic a tive of vari able in ten sity of leaching and for ma tion of the REE en rich ments (in clud ing MREE) by MREE>HREE>LREE flu ids, as ev i denced by the MREE-enriched sig na tures. Over print ing of sec ond ary en rich ments over the orig i nal REE pat tern due to re dis tri bu tion along the path ways of ex pand ing flu ids are pos tu lated to ac count for the ap par ent dif fer ences in the dis tri bu tion and con cen tra tion of REE (in clud ing the MREE-en riched trend) be tween the ox i dized rocks, cop per-bear ing rocks, and re duced lithologies bar ren in cop per.

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“…Hor i zon tal ar rangement of the de posit is dis rupted by a dis junc tive block tec tonic (Piestrzyñski and Salamon, 1986;K³apciñski and Peryt, 2007). For de tailed de scrip tion of the ge ol ogy, ore min er al ogy and or igin of the Cu-Ag de posit see Mayer and Piestrzyñski (1985), Wodzicki and Piestrzyñski (1994), Oszczepalski (1999); K³ap -ciñski and Peryt (2007), Piestrzyñski (2007a, b), Pieczonka et al (2008) and Pieczonka (2011).…”

Section: Geological Settingmentioning

confidence: 99%

I noticed you are using Open Journal Systems to publish and manage Geological Quarterly. I’ve heard from other editors how clunky it is, not to mention the burden of maintenance and system upgrades. Does this feeling resonate with you? If so, I would be interested to hear about your experience and put Scholastica on your radar as an alternative to OJS. Do you have time next week for a quick chat?

Kozub‐Budzyń¹,

Piestrzyński²

2018

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Kozub-Budzyñ, G.A., Piestrzyñski, A., 2018. The first oc cur rence of cupropearceite in the Kupferschiefer de posit, Lubin mine, SW Po land. Geo log i cal Quar terly, 62 (2): 319-326, doi: 10.7306/gq.1407As so ci ate ed i tor: S³awomir Oszczepalski Cupropearceite is a sulphosalt be long ing to the pearceite-polybasite group, formed due to Cu-for-Ag sub sti tu tion. It is a rare min eral of the Earth's crust, de scribed only in four lo ca tions so far. This work re ports the oc cur rence of cupropearceite in the up per part of the Weissliegend sand stone from the Cu-Ag de posit in the Fore-Sudetic Monocline. The min eral is as so ci ated with stromeyerite, bornite, chalcocite, na tive sil ver, sil ver amal gams and, rarely, py rite. For ma tion of cupropearceite is related to fluid ac tiv ity dur ing low-tem per a ture hy dro ther mal events re spon si ble for the for ma tion of the Cu-Ag ore min er alization. The iden ti fi ca tion of cupropearceite is im por tant in terms of con strain ing min er als bear ing as so ci ated met als, par tic u larly Ag and As. This work also pres ents oc cur rence of this rare min eral in the pre vi ously un noted min eral as sem blage men tioned above. The pres ence of cupropearceite con firms a low-tem per a ture, hy dro ther mal or i gin of the Cu-Ag de posit in the Fore-Sudetic Monocline.

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An ore genetic model for the Lubin—Sieroszowice mining district, Poland

Cited by 57 publications

References 42 publications

A multistage origin for Kupferschiefer mineralization

A multistage origin for Kupferschiefer mineralization

Controls on the distribution of rare earth elements in the Kupferschiefer series of SW Poland

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