[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:6928":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":9,"nolocadd":13,"blacklisted":13,"mindat_formula":14,"mindat_formula_note":15,"ima_formula":16,"elements":17,"sigelements":24,"key_elements":25,"impurities":11,"cim":11,"ima_status":26,"ima_notes":11,"ima_history":11,"approval_year":28,"publication_year":11,"discovery_year":11,"strunz10ed1":29,"strunz10ed2":30,"strunz10ed3":30,"strunz10ed4":11,"dana8ed1":30,"dana8ed2":30,"dana8ed3":30,"dana8ed4":30,"csystem":31,"cclass":32,"spacegroup":33,"spacegroupset":34,"a":35,"b":36,"c":37,"alpha":30,"beta":38,"gamma":30,"aerror":11,"berror":11,"cerror":11,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":39,"csmetamict":13,"commentcrystal":11,"twinning":11,"tranglide":11,"parting":40,"epitaxidescription":11,"morphology":11,"tlform":41,"hmin":42,"hmax":42,"hardtype":11,"vhnmin":30,"vhnmax":30,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":43,"dmeas2":43,"dcalc":44,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":45,"commentluster":11,"diapheny":46,"streak":47,"colour":48,"commentcolor":11,"colors":49,"streak_colors":55,"luminescence":11,"uv":11,"cleavage":56,"cleavagetype":57,"fracturetype":58,"tenacity":59,"commentbreak":11,"opticaltype":60,"opticalsign":61,"opticalalpha":62,"opticalalpha2":30,"opticalalphaerror":39,"opticalbeta":63,"opticalbeta2":30,"opticalbetaerror":39,"opticalgamma":64,"opticalgamma2":30,"opticalgammaerror":39,"opticalomega":30,"opticalomega2":30,"opticalomegaerror":11,"opticalepsilon":30,"opticalepsilon2":30,"opticalepsilonerror":11,"opticaln":30,"opticaln2":30,"opticalnerror":11,"optical2vcalc":65,"optical2vcalc2":30,"optical2vcalcerror":11,"optical2vmeasured":66,"optical2vmeasured2":30,"optical2vmeasurederror":67,"rimin":68,"rimax":69,"opticaldispersion":70,"opticalpleochroism":71,"opticalpleochorismdesc":72,"opticalbirefringence":11,"opticalcomments":73,"opticalcolour":11,"opticalinternal":11,"opticaltropic":11,"opticalanisotropism":11,"opticalbireflectance":11,"opticalextinction":11,"opticalr":11,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":11,"industrial":11,"occurrence":74,"otheroccurrence":11,"type_specimen_store":75,"description_short":11,"aboutname":76,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":77,"reviewed_at":11,"variety_of":11,"varieties":78,"group_members":79,"associates":86,"confused_with":87,"type_localities":88,"occurrence_total":89,"citations":90,"images":115,"structures":116,"synonyms":123,"language_names":127,"wikidata_qid":146,"texts":147},6928,"1:1:6928:7","65cccc06-21b8-4bdf-a180-7b322c855a5d","Clino-ferri-holmquistite","Cfhlm",0,"mineral",null,1513,false,"◻Li\u003Csub>2\u003C\u002Fsub>(Mg\u003Csub>3\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>)(Si\u003Csub>8\u003C\u002Fsub>O\u003Csub>22\u003C\u002Fsub>)(OH)\u003Csub>2\u003C\u002Fsub>","The clino-holmquistite group minerals are monoclinic lithium amphiboles defined with: \r\n\u003Csup>A\u003C\u002Fsup>(Na+K+2Ca)\u003C 0.5 apfu,\r\n\u003Csup>C\u003C\u002Fsup>Li \u003C 0,5 apfu\r\n\r\nClino-ferri-holmquistite is defined with \r\nC\u003Csup>2+\u003C\u002Fsup> position: Mg dominant\r\nC\u003Csup>3+\u003C\u002Fsup> position: Fe dominant\r\nW position: (OH) dominant","◻Li\u003Csub>2\u003C\u002Fsub>(Mg\u003Csub>3\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>)Si\u003Csub>8\u003C\u002Fsub>O\u003Csub>22\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub>",[18,19,20,21,22,23],"Fe","Li","Mg","Si","O","H",[18,19,20,21,22,23],[19],[27],"APPROVED",2014,"9","0","Monoclinic",5,11,"C2\u002Fm ","9.48","17.845","5.283","102.03",2,"a (001) parting","Ferri-clinoholmquistite has two grain-size subpopulations: Crystals in the intergranular aggregates average 0.15(10) mm in length and 0.11(6) mm in width, whereas micro-inclusions in albite, microcline, quartz, and titanite are 0.11(13) mm in length and 0.03(2) mm in width.\r\nThe crystals have prismatic habit, elongated up to 0.5 mm along [001]",6,"3.19","3.25","Vitreous","Translucent","grey","Black",[50,51,52,53,54],"black","gray","yellow","green","blue",[51],"{110}","Perfect","Splintery","brittle","Biaxial","+","1.699","1.703","1.708","83","72",7,1.699,1.708,"relatively strong","Strong","X = yellow green, Y = indigo blue and Z = green blue","shows anomalous indigo and brown interference colors.","Hydrothermal epi-syenite bodies\r\nderived from a Li-rich cordierite-bearing porphyritic granite","Museu Nacional de Ciencias Naturales, Madrid Spain","The original material used to describe clino-ferri-holmquistite (IMA1995-045) by Caballero et al (1998) (originally named by them as \"ferri-clinoholmquistite\") was renamed \"sodic-ferri-clinoholmquistite\" and finally became \u003Cm>Clino-ferro-ferri-holmquistite\u003C\u002Fm>, its current valid name.\r\n\r\nThe mineral now named clino-ferri-holmquistite was originally published as ferri-ottoliniite (IMA2001-067) in 2001. In the 2012 amphibole nomenclature, its composition was considered intermediate between clino-ferri-holmquistite and magnesio-riebeckite, and the ottoliniite root name is discredited.\r\n\r\nThe clino-ferri-holmquistite holotype material empirical formula is A(K0.07Na0.38)B(Na0.70Li1.24Ca0.06)C(Mg1.35Fe2+0.92Mn2+0.13 Zn0.31Fe3+1.71Al0.10Ti0.06Li0.42) Si8 O22 (OH1.51F0.47). As  Li>Na in the B position the mineral is considered a clino-ferri-holmquistite, which was approved in september 2014 (Proposal 14-G ).","2026-05-14 03:38:27",[],[80],{"id":81,"name":82,"entrytype":9,"csystem":31,"ima_formula":83,"mindat_formula":84,"hmin":42,"hmax":42,"dmeas":30,"dcalc":85,"primary_image_id":11},6927,"Clino-ferro-ferri-holmquistite","◻Li\u003Csub>2\u003C\u002Fsub>(Fe\u003Csup>2+\u003C\u002Fsup>\u003Csub>3\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>)Si\u003Csub>8\u003C\u002Fsub>O\u003Csub>22\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub>","◻Li\u003Csub>2\u003C\u002Fsub>(Fe\u003Csup>2+\u003C\u002Fsup>\u003Csub>3\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>)(Si\u003Csub>8\u003C\u002Fsub>O\u003Csub>22\u003C\u002Fsub>)(OH)\u003Csub>2\u003C\u002Fsub>","3.24",[],[],[],1,[91,96,101,105,110],{"id":92,"year":93,"html":94,"doi":95},393691,1998,"Caballero, Jose M., Monge, Angeles, La Iglesia, Angel, Tornos, Fernando (1998) Ferri-clinoholmquistite, Li\u003Csub>2\u003C\u002Fsub>(Fe\u003Csup>2+\u003C\u002Fsup>,Mg)\u003Csub>3\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>Si\u003Csub>8\u003C\u002Fsub>O\u003Csub>22\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub>, a new \u003Csup>B\u003C\u002Fsup>Li clinoamphibole from the Pedriza Massif, Sierra de Guadarrama, Spanish Central System. \u003Ci>American Mineralogist\u003C\u002Fi>,  83 (1) 167-171 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam-1998-1-217'>doi:10.2138\u002Fam-1998-1-217\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fam\u002Fvol83\u002FAM83_167.pdf' class='refpdflink'>\u003C\u002Fa>","10.2138\u002Fam-1998-1-217",{"id":97,"year":98,"html":99,"doi":100},395062,2004,"Oberti, Roberta, Cámara, Fernando, Caballero, José Maria (2004) Ferri-ottoliniite and ferriwhittakerite, two new end-members of the new Group 5 for monoclinic amphiboles. \u003Ci>American Mineralogist\u003C\u002Fi>,  89 (5) 888-893 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam-2004-5-624'>doi:10.2138\u002Fam-2004-5-624\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fam\u002Fvol89\u002FAM89_888.pdf' class='refpdflink'>\u003C\u002Fa>","10.2138\u002Fam-2004-5-624",{"id":102,"year":98,"html":103,"doi":104},153095,"Iezzi, G., Cámara, F., Oberti, R., Ventura, G. Della, Pedrazzi, G., Robert, J.-L. (2004) Synthesis, crystal structure and crystal chemistry of ferri-clinoholmquistite, □Li\u003Csub>2\u003C\u002Fsub>Mg\u003Csub>3\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>Si\u003Csub>8\u003C\u002Fsub>O\u003Csub>22\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub>. \u003Ci>Physics and Chemistry of Minerals\u003C\u002Fi>,  31 (6)  \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs00269-004-0402-2'>doi:10.1007\u002Fs00269-004-0402-2\u003C\u002Fa>","10.1007\u002Fs00269-004-0402-2",{"id":106,"year":107,"html":108,"doi":109},64226,2006,"Hawthorne, F. C., Oberti, R. (2006) On the classification of amphiboles. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  44 (1) 1-21 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2113\u002Fgscanmin.44.1.1'>doi:10.2113\u002Fgscanmin.44.1.1\u003C\u002Fa>","10.2113\u002Fgscanmin.44.1.1",{"id":111,"year":112,"html":113,"doi":114},396910,2012,"Hawthorne, F. C., Oberti, R., Harlow, G. E., Maresch, W. V., Martin, R. F., Schumacher, J. C., Welch, M. D. (2012) Nomenclature of the amphibole supergroup. \u003Ci>American Mineralogist\u003C\u002Fi>,  97 (11) 2031-2048 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam.2012.4276'>doi:10.2138\u002Fam.2012.4276\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Frruff_1.0\u002Fuploads\u002FAM97_2031.pdf' class='refpdflink'>\u003C\u002Fa>","10.2138\u002Fam.2012.4276",[],[117],{"id":118,"url":119,"label":120,"formula":121,"spacegroup":122,"year":98},2809,"\u002Fcif\u002F2809.cif","Oberti 2004","Na1.376 K.125 Mg1.35 Fe2.63 Zn.31 Al.1 Ti.06 Li1.66 Mn.13 Ca.06 Si8 H1.51 O23.51 F.47","C 1 2\u002Fm 1",[124,125,126],"Clino-ferri-holmquistiet","IMA2001-067","IMA2001-067a",[128,132,137,141],{"lang":129,"names":130},"ca",[131],"clinoferriholmquistita",{"lang":133,"names":134},"de",[135,136],"IMA 2001-067a","Klino-Ferri-Holmquistit",{"lang":138,"names":139},"eu",[140],"Klino-ferri-holmquistita",{"lang":142,"names":143},"it",[144,145],"clino-ferri-holmquistite","ferri-ottoliniite","Q3743171",{"history":11,"applications":11}]