[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:1135":3},{"id":4,"longid":5,"guid":6,"name":7,"shortcode_ima":8,"entrytype":9,"entrytype_text":10,"varietyof":11,"synid":11,"polytypeof":11,"groupid":12,"weighting":13,"nolocadd":14,"blacklisted":14,"mindat_formula":15,"mindat_formula_note":11,"ima_formula":16,"elements":17,"sigelements":24,"key_elements":11,"impurities":25,"cim":26,"ima_status":27,"ima_notes":11,"ima_history":11,"approval_year":11,"publication_year":30,"discovery_year":31,"strunz10ed1":32,"strunz10ed2":33,"strunz10ed3":34,"strunz10ed4":35,"dana8ed1":36,"dana8ed2":37,"dana8ed3":38,"dana8ed4":39,"csystem":40,"cclass":11,"spacegroup":11,"spacegroupset":41,"a":42,"b":43,"c":44,"alpha":41,"beta":41,"gamma":41,"aerror":11,"berror":11,"cerror":11,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":11,"csmetamict":14,"commentcrystal":45,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":46,"tlform":47,"hmin":48,"hmax":49,"hardtype":11,"vhnmin":41,"vhnmax":41,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":41,"dmeas2":41,"dcalc":41,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":50,"commentluster":51,"diapheny":52,"streak":53,"colour":54,"commentcolor":11,"colors":55,"streak_colors":61,"luminescence":11,"uv":11,"cleavage":62,"cleavagetype":63,"fracturetype":64,"tenacity":65,"commentbreak":11,"opticaltype":66,"opticalsign":67,"opticalalpha":68,"opticalalpha2":69,"opticalalphaerror":11,"opticalbeta":70,"opticalbeta2":71,"opticalbetaerror":11,"opticalgamma":70,"opticalgamma2":71,"opticalgammaerror":11,"opticalomega":41,"opticalomega2":41,"opticalomegaerror":11,"opticalepsilon":41,"opticalepsilon2":41,"opticalepsilonerror":11,"opticaln":41,"opticaln2":41,"opticalnerror":11,"optical2vcalc":41,"optical2vcalc2":41,"optical2vcalcerror":11,"optical2vmeasured":41,"optical2vmeasured2":72,"optical2vmeasurederror":11,"rimin":73,"rimax":74,"opticaldispersion":75,"opticalpleochroism":11,"opticalpleochorismdesc":11,"opticalbirefringence":76,"opticalcomments":11,"opticalcolour":11,"opticalinternal":11,"opticaltropic":11,"opticalanisotropism":11,"opticalbireflectance":11,"opticalextinction":11,"opticalr":11,"specdispm":11,"ir":77,"electrical":11,"magnetism":11,"thermalbehaviour":78,"other":11,"industrial":11,"occurrence":79,"otheroccurrence":11,"type_specimen_store":80,"description_short":81,"aboutname":82,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":83,"reviewed_at":11,"variety_of":11,"varieties":84,"group_members":85,"associates":108,"confused_with":109,"type_localities":110,"occurrence_total":117,"citations":118,"images":209,"structures":220,"synonyms":221,"language_names":225,"wikidata_qid":249,"texts":250},1135,"1:1:1135:4","74558b9a-c91f-4d4c-af27-6ab5ed26e63b","Corrensite","Crr",0,"mineral",null,470677,217,false,"(Mg,Fe)\u003Csub>9\u003C\u002Fsub>((Si,Al)\u003Csub>8\u003C\u002Fsub>O\u003Csub>20\u003C\u002Fsub>)(OH)\u003Csub>10\u003C\u002Fsub>·nH\u003Csub>2\u003C\u002Fsub>O","(Ca,Na,K)\u003Csub>1-x\u003C\u002Fsub>(Mg,Fe,Al)\u003Csub>9\u003C\u002Fsub>(Si,Al)\u003Csub>8\u003C\u002Fsub>O\u003Csub>20\u003C\u002Fsub>(OH)\u003Csub>10\u003C\u002Fsub> · nH\u003Csub>2\u003C\u002Fsub>O",[18,19,20,21,22,23],"Al","Fe","Mg","Si","O","H",[20,21,22,23],",Ti,Fe,Mn,K,,","16.19.23",[28,29],"APPROVED","GRANDFATHERED",1954,"1954","9","E","C","60","71","4","2","5","Orthorhombic","0","5.337","9.215","29.0","Various unit cells have been proposed including hexagonal, also monoclinic","Fine-grained, occasionally as barely visible flakes.","Dense fine-grained mixtures, also thin dustings on late minerals in cavities",1,2,"Waxy,Dull,Earthy","Low luster due to fine-grained particles","Translucent","White to light gray","Dark green, Yellow green,Blackish green, Brown, Light golden brown, gray white",[56,57,58,59,60],"green","brown","yellow","gray","white",[60,59],"{001} perfect, but rarely visible on casual inspection due to small particle size.","Perfect","Micaceous","flexible","Biaxial","-","1.56","1.585","1.582","1.612","10",1.56,1.612,"r \u003C v strong","May be 0.01-0.03, but 0.00 reported","Clays and Clay Minerals 33:458 (1985).","HLC corrensite basal spacings collapse to 24 Angstroms at 500 degrees C.","Found in pelitic sediments, also in evaporites, marbles, also late stage hydrothermal coatings in basalts, etc. Corrensite may persist through chlorite grade metamorphism.","National Museum of Natural History, Washington, D.C., USA, numbers 107373, 162265.","A 1:1 regular interstratification of a trioctahedral chlorite with either a trioctahedral vermiculite (low layer charge corrensite, LLC) or a trioctahedral smectite (high layer charge corrensite, HLC).","Named by Friedrich Lippmann in 1954 in honor of Carl Wilhelm Correns (19 May 1893, Tübingen, Germany - 29 August 1980, Göttingen, Germany), professor of mineralogy and petrography in the University of Göttingen, Germany and Director of the Sedimentary Petrology Institute. He received the Roebling Medal in 1976.","2025-12-07 18:32:05",[],[86,93,101],{"id":87,"name":88,"entrytype":9,"csystem":89,"ima_formula":90,"mindat_formula":91,"hmin":48,"hmax":49,"dmeas":41,"dcalc":41,"primary_image_id":92},115,"Aliettite","Monoclinic","Ca\u003Csub>0.2\u003C\u002Fsub>Mg\u003Csub>6\u003C\u002Fsub>(Si,Al)\u003Csub>8\u003C\u002Fsub>O\u003Csub>20\u003C\u002Fsub>(OH)\u003Csub>4\u003C\u002Fsub> · 4H\u003Csub>2\u003C\u002Fsub>O","Ca\u003Csub>0.2\u003C\u002Fsub>Mg\u003Csub>6\u003C\u002Fsub>((Si,Al)\u003Csub>8\u003C\u002Fsub>O\u003Csub>20\u003C\u002Fsub>)(OH)\u003Csub>4\u003C\u002Fsub>·4H\u003Csub>2\u003C\u002Fsub>O",661,{"id":94,"name":95,"entrytype":9,"csystem":89,"ima_formula":96,"mindat_formula":97,"hmin":98,"hmax":48,"dmeas":41,"dcalc":99,"primary_image_id":100},3377,"Rectorite","(Na,Ca)Al\u003Csub>4\u003C\u002Fsub>(Si,Al)\u003Csub>8\u003C\u002Fsub>O\u003Csub>20\u003C\u002Fsub>(OH)\u003Csub>4\u003C\u002Fsub> · 2H\u003Csub>2\u003C\u002Fsub>O","(Na,Ca)Al\u003Csub>4\u003C\u002Fsub>((Si,Al)\u003Csub>8\u003C\u002Fsub>O\u003Csub>20\u003C\u002Fsub>)(OH)\u003Csub>4\u003C\u002Fsub>·2H\u003Csub>2\u003C\u002Fsub>O",0.5,"2.34",20648,{"id":102,"name":103,"entrytype":9,"csystem":89,"ima_formula":104,"mindat_formula":105,"hmin":48,"hmax":49,"dmeas":106,"dcalc":41,"primary_image_id":107},4001,"Tosudite","Na\u003Csub>0.5\u003C\u002Fsub>(Al,Mg)\u003Csub>6\u003C\u002Fsub>(Si,Al)\u003Csub>8\u003C\u002Fsub>O\u003Csub>18\u003C\u002Fsub>(OH)\u003Csub>12\u003C\u002Fsub> · 5H\u003Csub>2\u003C\u002Fsub>O","Na\u003Csub>0.5\u003C\u002Fsub>(Al,Mg)\u003Csub>6\u003C\u002Fsub>((Si,Al)\u003Csub>8\u003C\u002Fsub>O\u003Csub>18\u003C\u002Fsub>)(OH)\u003Csub>12\u003C\u002Fsub>·5H\u003Csub>2\u003C\u002Fsub>O","2.83",83435,[],[],[111],{"id":112,"txt":113,"latitude":114,"longitude":115,"country":116},23023,"Zaisersweiher quarry, Maulbronn, Enzkreis, Karlsruhe Region, Baden-Württemberg, Germany",48.9988135,8.8478518,"Germany",65,[119,123,128,132,136,140,144,148,153,157,161,166,171,176,181,185,190,194,199,204],{"id":120,"year":30,"html":121,"doi":122},16186818,"Lippmann, Friedrich (1954) Über einen Keuperton von Zaisersweiher bei Maulbronn. \u003Ci>Heidelberger Beiträge zur Mineralogie und Petrographie\u003C\u002Fi>,  4 (1-2). 130-134 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1007\u002Fbf01111150'>doi:10.1007\u002Fbf01111150\u003C\u002Fa>","10.1007\u002Fbf01111150",{"id":124,"year":125,"html":126,"doi":127},561926,1960,"Martin Vivaldi, J. L. (1960) Corrensite and Swelling Chlorite. \u003Ci>Clay Minerals\u003C\u002Fi>,  4 (24) 173-181 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fclaymin.1960.004.24.02'>doi:10.1180\u002Fclaymin.1960.004.24.02\u003C\u002Fa>","10.1180\u002Fclaymin.1960.004.24.02",{"id":129,"year":130,"html":131,"doi":11},523572,1961,"Fleischer, M. (1961) New mineral names. \u003Ci>American Mineralogist\u003C\u002Fi>,  46 (5-6). 765-770 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM46\u002FAM46_765.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":133,"year":134,"html":135,"doi":11},526292,1974,"Kopp, Otto C., Fallis, and Susan M. (1974) Corrensite in the Wellington Formation, Lyons, Kansas. \u003Ci>American Mineralogist\u003C\u002Fi>,  59 (5-6) 623-624 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM59\u002FAM59_623.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":137,"year":138,"html":139,"doi":11},526548,1975,"Furbish, William J. (1975) Corrensite of deuteric origin. \u003Ci>American Mineralogist\u003C\u002Fi>,  60 (9-10) 928-930 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM60\u002FAM60_928.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":141,"year":142,"html":143,"doi":11},16106604,1981,"Bailey, S.W. (1981) A system of nomenclature for regular interstratifications. The Canadian Mineralogist: 19: 651-655.",{"id":145,"year":146,"html":147,"doi":11},15962490,1982,"Bailey, S.W. (1982) Nomenclature for regular interstratifications. American Mineralogist: 67: 394-398.",{"id":149,"year":150,"html":151,"doi":152},146290,1987,"De Kimpe, C. R.; Miles, N.; Kodama, H.; Dejou, J. (1987) Alteration of Phlogopite to Corrensite at Sharbot Lake, Ontario. \u003Ci>Clays and Clay Minerals\u003C\u002Fi>,  35 (2). 150-158 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1346\u002Fccmn.1987.0350207'>doi:10.1346\u002Fccmn.1987.0350207\u003C\u002Fa>","10.1346\u002Fccmn.1987.0350207",{"id":154,"year":155,"html":156,"doi":11},16106605,1988,"De Kimpe, C.R., Miles, N.M. (1988) Geographic distribution of corrensite and associated minerals in southeastern Ontario. The Canadian Mineralogist: 26: 957-964.",{"id":158,"year":155,"html":159,"doi":160},2572601,"MILES, N. M., KIMPE, C. R. De (1988) SIGNIFICANCE OF CORRENSITE IN SOILS OF SOUTHEASTERN ONTARIO. \u003Ci>Canadian Journal of Soil Science\u003C\u002Fi>, 68 (3). 671-681 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.4141\u002Fcjss88-060'>doi:10.4141\u002Fcjss88-060\u003C\u002Fa>","10.4141\u002Fcjss88-060",{"id":162,"year":163,"html":164,"doi":165},76508,1990,"Shau, Yen-Hong, Peacor, Donald R., Essene, Eric J. (1990) Corrensite and mixed-layer chlorite\u002Fcorrensite in metabasalt from northern Taiwan: TEM\u002FAEM, EMPA, XRD, and optical studies. \u003Ci>Contributions to Mineralogy and Petrology\u003C\u002Fi>,  105 (2) 123-142 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1007\u002Fbf00678980'>doi:10.1007\u002Fbf00678980\u003C\u002Fa>","10.1007\u002Fbf00678980",{"id":167,"year":168,"html":169,"doi":170},146665,1991,"Lindqvist, Kristian (1991) Corrensite of Hydrothermal Origin from Veitsivaara, Eastern Finland. \u003Ci>Clays and Clay Minerals\u003C\u002Fi>,  39 (2) 219-223 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1346\u002Fccmn.1991.0390214'>doi:10.1346\u002Fccmn.1991.0390214\u003C\u002Fa>","10.1346\u002Fccmn.1991.0390214",{"id":172,"year":173,"html":174,"doi":175},147108,1995,"Dubińska, Elżbieta (1995) Corrensite from Nasławice (Lower Silesia, Poland): Some Problems of Mineral Identification and Origin. \u003Ci>Clays and Clay Minerals\u003C\u002Fi>,  43 (5) 630-636 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1346\u002Fccmn.1995.0430513'>doi:10.1346\u002Fccmn.1995.0430513\u003C\u002Fa>","10.1346\u002Fccmn.1995.0430513",{"id":177,"year":178,"html":179,"doi":180},393552,1997,"Beaufort, Daniel; Baronnet, Alain; Lanson, Bruno; Meunier, Alain (1997) Corrensite; a single phase or a mixed-layer phyllosilicate in saponite-to-chlorite conversion series? A case study of Sancerre-Couy deep drill hole (France). \u003Ci>American Mineralogist\u003C\u002Fi>,  82 (1-2). 109-124 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam-1997-1-213'>doi:10.2138\u002Fam-1997-1-213\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fam\u002Fvol82\u002FAM82_109.pdf' class='refpdflink'>\u003C\u002Fa>","10.2138\u002Fam-1997-1-213",{"id":182,"year":178,"html":183,"doi":184},563551,"Garvie, L. A. J., Metcalfe, R. (1997) A vein occurrence of co-existing talc, saponite, and corrensite, Builth Wells, Wales. \u003Ci>Clay Minerals\u003C\u002Fi>,  32 (2) 223-240 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fclaymin.1997.032.2.05'>doi:10.1180\u002Fclaymin.1997.032.2.05\u003C\u002Fa>","10.1180\u002Fclaymin.1997.032.2.05",{"id":186,"year":187,"html":188,"doi":189},147408,1998,"Li, Gejing; Peacor, Donald R.; Essene, Eric J. (1998) The Formation of Sulfides During Alteration of Biotite to Chlorite-Corrensite. \u003Ci>Clays and Clay Minerals\u003C\u002Fi>,  46 (6). 649-657 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1346\u002Fccmn.1998.0460605'>doi:10.1346\u002Fccmn.1998.0460605\u003C\u002Fa>","10.1346\u002Fccmn.1998.0460605",{"id":191,"year":192,"html":193,"doi":11},16963807,2001,"(2001) Corrensite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fcorrensite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":195,"year":196,"html":197,"doi":198},397275,2013,"Kogure, T., Drits, V. A., Inoue, S. (2013) Structure of mixed-layer corrensite-chlorite revealed by high-resolution transmission electron microcopy (HRTEM) \u003Ci>American Mineralogist\u003C\u002Fi>,  98 (7) 1253-1260 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam.2013.4314'>doi:10.2138\u002Fam.2013.4314\u003C\u002Fa>","10.2138\u002Fam.2013.4314",{"id":200,"year":201,"html":202,"doi":203},10366800,2016,"Kralj, Polona (2016) Hydrothermal alteration of chlorite to randomly interstratified corrensite-chlorite: Geological evidence from the Oligocene Smrekovec Volcanic Complex, Slovenia. \u003Ci>Applied Clay Science\u003C\u002Fi>, 134. 235-245 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.clay.2016.10.025'>doi:10.1016\u002Fj.clay.2016.10.025\u003C\u002Fa>","10.1016\u002Fj.clay.2016.10.025",{"id":205,"year":206,"html":207,"doi":208},16627683,2023,"Matýsek, Dalibor, Jirásek, Jakub (2023) Corrensite and associated smectites in the Teschenite Association Rocks from the Podbeskydí Area (Czech Republic and Poland). \u003Ci>Applied Clay Science\u003C\u002Fi>,  243. 107067 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.clay.2023.107067'>doi:10.1016\u002Fj.clay.2023.107067\u003C\u002Fa>","10.1016\u002Fj.clay.2023.107067",[210],{"id":211,"source_url":212,"license_code":213,"credit_html":214,"title":215,"description":216,"author":217,"original_width":218,"original_height":219},6343,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=189822886","CC BY 4.0","David Hospital, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=189822886\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Corrensite.jpg","Grey crystal aggregates of the rare mineral corrensite on a quartz matrix. From Luzerne County, Pennsylvania, United States of America. Ex Vandenbroucke Museum collection from Waregem, Belgium.","David Hospital",704,600,[],[222,223,224],"Corrensiet","HLC Corrensite","LLC Corrensite",[226,230,234,238,241,245],{"lang":227,"names":228},"ca",[229],"corrensita",{"lang":231,"names":232},"de",[233],"Corrensit",{"lang":235,"names":236},"eu",[237],"Corrensita",{"lang":239,"names":240},"it",[7],{"lang":242,"names":243},"uk",[244],"Коренсит",{"lang":246,"names":247},"zh",[248],"绿泥间蛭石","Q3694401",{"history":11,"applications":11}]