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Hallimondite, a new uranium mineral from the Michael Mine near Reichenbach (Black Forest, Germany)

The hallimondite occurs as small tabular crystals with triclinic symmetry and as fine-grained coatings in cavities and fissures in quartz, in association with hügelite and mimetite. Data on mode of occurrence, crystallography, and physical, optical, chemical, and x-ray properties are reported. The f...

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Published in:The American mineralogist 1965, Vol.50 (9), p.1143-1157
Main Author: Walenta, Kurt
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Language:English
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description The hallimondite occurs as small tabular crystals with triclinic symmetry and as fine-grained coatings in cavities and fissures in quartz, in association with hügelite and mimetite. Data on mode of occurrence, crystallography, and physical, optical, chemical, and x-ray properties are reported. The formula Pb2(UO2)(AsO4)2 was derived from synthetic material. Comparison with the lead uranyl phosphate mineral parsonsite shows hallimondite to be the arsenate analogue of parsonsite.
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Data on mode of occurrence, crystallography, and physical, optical, chemical, and x-ray properties are reported. The formula Pb2(UO2)(AsO4)2 was derived from synthetic material. 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Data on mode of occurrence, crystallography, and physical, optical, chemical, and x-ray properties are reported. The formula Pb2(UO2)(AsO4)2 was derived from synthetic material. Comparison with the lead uranyl phosphate mineral parsonsite shows hallimondite to be the arsenate analogue of parsonsite.</description><subject>Black Forest</subject><subject>Central Europe</subject><subject>crystal structure</subject><subject>crystal systems</subject><subject>Europe</subject><subject>Germany</subject><subject>hallimondite</subject><subject>mineral data</subject><subject>mineralogy</subject><subject>new mineral</subject><subject>Pb2(UO2)(AsO4)2</subject><subject>properties</subject><subject>triclinic system</subject><issn>0003-004X</issn><issn>1945-3027</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1965</creationdate><recordtype>article</recordtype><sourceid/><recordid>eNotj1FLwzAUhYMoWKf_IY-KK9wmTdM-6nCbMBFEwbdym9zazjSFtGP47xfRpw8OH-dwzliSVblKJQh9zhIAkClA_nnJrqZpDyCEVFXCmi061w-jt_1MS47c05EfAvr-MPCh9xTQ8TaMA5874i-96ZBcpKdoYuBvFCPyDZqO3z46NN98PQaa5iXfUBjQ_9xds4sW3UQ3_1ywj_XT-2qb7l43z6uHXYpZns-pNQ3oAgX9smyFLKk01khBBVZtoypQrS3AmCYT8RQiWpRaqyjnymqUC3b_1_tF42R68oaOY3C23o-H4ONynVWFrgGUFFKeAMqSVRU</recordid><startdate>1965</startdate><enddate>1965</enddate><creator>Walenta, Kurt</creator><general>Mineralogical Society of America</general><scope/></search><sort><creationdate>1965</creationdate><title>Hallimondite, a new uranium mineral from the Michael Mine near Reichenbach (Black Forest, Germany)</title><author>Walenta, Kurt</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a144t-dcb076a2ecb078f238e8cdc32e6a9fb5905fd60ccb12302aaada377507845d7a3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1965</creationdate><topic>Black Forest</topic><topic>Central Europe</topic><topic>crystal structure</topic><topic>crystal systems</topic><topic>Europe</topic><topic>Germany</topic><topic>hallimondite</topic><topic>mineral data</topic><topic>mineralogy</topic><topic>new mineral</topic><topic>Pb2(UO2)(AsO4)2</topic><topic>properties</topic><topic>triclinic system</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Walenta, Kurt</creatorcontrib><jtitle>The American mineralogist</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Walenta, Kurt</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Hallimondite, a new uranium mineral from the Michael Mine near Reichenbach (Black Forest, Germany)</atitle><jtitle>The American mineralogist</jtitle><date>1965</date><risdate>1965</risdate><volume>50</volume><issue>9</issue><spage>1143</spage><epage>1157</epage><pages>1143-1157</pages><issn>0003-004X</issn><eissn>1945-3027</eissn><abstract>The hallimondite occurs as small tabular crystals with triclinic symmetry and as fine-grained coatings in cavities and fissures in quartz, in association with hügelite and mimetite. Data on mode of occurrence, crystallography, and physical, optical, chemical, and x-ray properties are reported. The formula Pb2(UO2)(AsO4)2 was derived from synthetic material. Comparison with the lead uranyl phosphate mineral parsonsite shows hallimondite to be the arsenate analogue of parsonsite.</abstract><pub>Mineralogical Society of America</pub><tpages>15</tpages></addata></record>
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identifier ISSN: 0003-004X
ispartof The American mineralogist, 1965, Vol.50 (9), p.1143-1157
issn 0003-004X
1945-3027
language eng
recordid cdi_geoscienceworld_journals_1967_005323
source Full-Text Journals in Chemistry (Open access)
subjects Black Forest
Central Europe
crystal structure
crystal systems
Europe
Germany
hallimondite
mineral data
mineralogy
new mineral
Pb2(UO2)(AsO4)2
properties
triclinic system
title Hallimondite, a new uranium mineral from the Michael Mine near Reichenbach (Black Forest, Germany)
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