Abstract
SummarySome structural analogies found in tsumebite, vauquelinite, fornacite, and brackebuschite make it possible to place these secondary lead minerals in the same series with general formula Pb2MeII(Z)(XO4)(YO4), where MeII is a bivalent cation as Cu2+ or Mn2+, Z is the hydroxyl group or the water molecule, X is S, Cr, or V, and Y is P, As, or V. Some crystallochemical considerations are developed in order to explain how the replacement of these elements affects the crystal structure in these substances.
Cited by
22 articles.
订阅此论文施引文献
订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献
1. As-bearing new mineral species from Valletta mine, Maira Valley, Piedmont, Italy: IV. Lombardoite, Ba2Mn3+(AsO4)2(OH) and aldomarinoite, Sr2Mn3+(AsO4)2(OH), description and crystal structure;Mineralogical Magazine;2022-04-07
2. Copper Minerals at Vesuvius Volcano (Southern Italy): A Mineralogical Review;Minerals;2019-11-26
3. Minerals with Brackebuschite-Like Structures: A Novel Solid Solution System Involving Cr6+ and V5+;Geology of Ore Deposits;2017-12
4. As-bearing new mineral species from Valletta mine, Maira Valley, Piedmont, Italy: III. Canosioite, Ba2Fe3+(AsO4)2(OH), description and crystal structure;Mineralogical Magazine;2017-04
5. Redetermination of brackebuschite, Pb2Mn3+(VO4)2(OH);Acta Crystallographica Section E Crystallographic Communications;2016-02-06