Here neotocite pseudomorphs after alabandite crystals, associated with barite, were also found.
It shows a 3-mm group of well-formed crystals, associated with manganoan calcite, neotocite and weathered alabandite (which is probably the source of this element).
General appearance: Platy inclusions (up to 0.15 mm) in pyrrhotite and alabandite
and as aggregates of platy grains on pyrrhotite.
(*)Apatite Arsenic (*)Pb-As-S glass (*)Barite (*)Baumhauerite-2a (*)Bournonite (*)Calcite (*)Chalcopyrite Chatkalite Clinozoisite Geocronite Gratonite (*)Hutchinsonite Jamesonite Manganaxinite Marcas ire (*)Orpiment Realgar Robinsonite (*)Scheelite Seligmannite Stannite (*)Wurtzite
Late-stage mineralization on the northern margin of the deposit is represented by Fe-Mn-rich sphalerite, wurtzite (both the sphalerite and the wurtzite are deep brown in color), alabandite, rhodochrosite and rhodonite.
Alabandite (*)Apatite Argentite (*)Arsenopyrite (*)Barite Bornite Canfieldite Cassiterite Chalcocite/digenite Cosalite Emplectite Hessite Hocartite (*)Hubnerite Lillianite Native silver Natrolite Polybasite Pyrargyrite (*)Pyrrhotite) Rhodochrosite Rhodonite (*)Scheelite Stannite Stephanite Tungstenite Wittichenite (*)Wurtzite
Arsenopyrite Chalcopyrite Fluorite Jamesonite Marcasite (*)Orpiment Quartz Realgar Tennantite/Tetrahedrite
Ankerite Arsenopyrite Bournonite Djurleite Dolomite Emplectite Famatinite Greenockite Gypsum Luzonite Marcasite Matildite Native arsenic Proustite Pyrrhotite (*)Siderite Stromeyerite (*)Vivianite
At Nordmark, an iron ore field consisting of several mines with some small manganese orebodies has yielded specimens as well; dump and in situ finds of several interesting minerals have been made, including rare manganese arsenates such as synadelphite, hematolite and allactite in small but attractive micromounts; also filipstadtite, manganostibite, katoptrite and alabandite. In different limestone-dolomite associations the boron-rich minerals harkerite, ludwigite and fluoborite have been identified, though not together.
Specially notable are microcrystals of samsonite, pyrostilpnite and pyrargyrite, large masses of alabandite, crude pinkish gray crystals of wenkite up to 1 cm and apophyllite in colorless to white crystals up to 2 cm, rarely associated with white harmotome crystals of the same size.
From the Urals, were masses of nearly pure scaly paragonite from Slyudorudnik, Vyshtym; pecoraite from Tscheremschanskoe; sonolite, alleghanyite, rhodonite, and alabandite
from Inyltschek, Kyrgy; tobermorite, from Bazberovskoe; sellaite from Suranskoe, Bashkirien; and clintonite, from Shishimskie Gory.