[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:52849":3},{"id":4,"longid":5,"guid":6,"name":7,"shortcode_ima":8,"entrytype":9,"entrytype_text":10,"varietyof":11,"synid":8,"polytypeof":8,"groupid":8,"weighting":12,"nolocadd":13,"blacklisted":13,"mindat_formula":8,"mindat_formula_note":8,"ima_formula":8,"elements":14,"sigelements":16,"key_elements":8,"impurities":8,"cim":8,"ima_status":8,"ima_notes":8,"ima_history":8,"approval_year":8,"publication_year":8,"discovery_year":8,"strunz10ed1":17,"strunz10ed2":17,"strunz10ed3":17,"strunz10ed4":8,"dana8ed1":8,"dana8ed2":8,"dana8ed3":8,"dana8ed4":8,"csystem":8,"cclass":8,"spacegroup":8,"spacegroupset":17,"a":8,"b":8,"c":8,"alpha":8,"beta":8,"gamma":8,"aerror":8,"berror":8,"cerror":8,"alphaerror":8,"betaerror":8,"gammaerror":8,"va3":8,"z":8,"csmetamict":13,"commentcrystal":8,"twinning":8,"tranglide":8,"parting":8,"epitaxidescription":8,"morphology":8,"tlform":8,"hmin":8,"hmax":8,"hardtype":8,"vhnmin":8,"vhnmax":8,"vhnerror":8,"vhng":8,"vhns":8,"commenthard":8,"dmeas":8,"dmeas2":8,"dcalc":8,"dmeaserror":8,"dcalcerror":8,"commentdense":8,"lustre":8,"lustretype":8,"commentluster":8,"diapheny":8,"streak":8,"colour":8,"commentcolor":8,"colors":8,"streak_colors":8,"luminescence":8,"uv":8,"cleavage":8,"cleavagetype":8,"fracturetype":8,"tenacity":8,"commentbreak":8,"opticaltype":8,"opticalsign":8,"opticalalpha":8,"opticalalpha2":8,"opticalalphaerror":8,"opticalbeta":8,"opticalbeta2":8,"opticalbetaerror":8,"opticalgamma":8,"opticalgamma2":8,"opticalgammaerror":8,"opticalomega":8,"opticalomega2":8,"opticalomegaerror":8,"opticalepsilon":8,"opticalepsilon2":8,"opticalepsilonerror":8,"opticaln":8,"opticaln2":8,"opticalnerror":8,"optical2vcalc":8,"optical2vcalc2":8,"optical2vcalcerror":8,"optical2vmeasured":8,"optical2vmeasured2":8,"optical2vmeasurederror":8,"rimin":8,"rimax":8,"opticaldispersion":8,"opticalpleochroism":8,"opticalpleochorismdesc":8,"opticalbirefringence":8,"opticalcomments":8,"opticalcolour":8,"opticalinternal":8,"opticaltropic":8,"opticalanisotropism":8,"opticalbireflectance":8,"opticalextinction":8,"opticalr":8,"specdispm":8,"ir":8,"electrical":8,"magnetism":8,"thermalbehaviour":8,"other":8,"industrial":8,"occurrence":8,"otheroccurrence":8,"type_specimen_store":8,"description_short":8,"aboutname":8,"rock_parent":8,"rock_parent2":8,"rock_root":18,"rock_bgs_code":8,"meteoritical_code":8,"updttime":19,"reviewed_at":8,"variety_of":20,"varieties":22,"group_members":23,"associates":24,"confused_with":25,"type_localities":26,"occurrence_total":18,"citations":27,"images":31,"structures":92,"synonyms":93,"language_names":94,"wikidata_qid":8,"texts":95},52849,"1:1:52849:6","15c11662-c674-4375-806b-cccab364ceca","Framesite",null,2,"variety",7473,20,false,[15],"C",[15],"0",0,"2025-08-11 12:15:20",{"id":11,"name":21,"entrytype":9,"csystem":8,"ima_formula":8,"mindat_formula":15,"hmin":8,"hmax":8,"dmeas":17,"dcalc":8,"strunz10ed1":17,"primary_image_id":8},"Bort",[],[],[],[],[],[28],{"id":29,"year":8,"html":30,"doi":8},16129323,"A.G.I. & A.G.I. Supp. = American Geological Institute. Glossary of Geology and Related Sciences. Washington, DC., 1957m 325 pp; supplement, 1960, 72 pp.",[32,42,49,56,63,71,78,85],{"id":33,"source_url":34,"license_code":35,"credit_html":36,"title":37,"description":38,"author":39,"original_width":40,"original_height":41},55675,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=84622242","CC BY 2.0","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=84622242\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Framesite diamondite (South Africa) 1 (49170199147).jpg","\u003Cp>(65.63 carats; ~2.3 centimeters across at its widest)\n\u003C\u002Fp>\n\u003Chr>\n\u003Cp>Diamondites are very rare, monomineralic diamond rocks.  \"Diamond\" is the name of a mineral and gemstone.  \"Diamondite\" is a rock name.  Several named varieties of diamondites exist, based on physical characteristics - for example, carbonado, framesite, stewardite, and yakutite.\n\u003C\u002Fp>\u003Cp>Seen here is a large framesite diamondite from South Africa.  The specific provenance has not been preserved, but according to the published literature, framesite is often produced from the Premier Mine and the Venetia Mine in South Africa (Heaney et al., 2005).\n\u003C\u002Fp>\u003Cp>Framesite is a granular, crystalline-textured diamondite.  Unlike carbonado diamondites (see elsewhere in this photo album), framesite is not cryptocrystalline - the crystals here are much larger.  The rock has a mix of large and small crystals (this would be called porphyritic in a granite).\n\u003C\u002Fp>\u003Cp>Locality: unrecorded\u002Fundisclosed mine in South Africa.\n\u003C\u002Fp>\n\u003Chr>\n\u003Cp>Some framesite references:\n\u003C\u002Fp>\u003Cp>Kurat & Dobosi (2000) - Garnet and diopside-bearing diamondites (framesites).  Mineralogy and Petrology 69: 143-159.\n\u003C\u002Fp>\u003Cp>Heaney et al. (2005) - Strange diamonds: the mysterious origins of carbonado and framesite.  Elements 1: 85-89.\n\u003C\u002Fp>\nTappert & Tappert (2011) - Chapter 2: the morphology of diamonds.  pp. 15-42 in  Diamonds in Nature: a Guide to Rough Diamonds.","James St. John",1580,1307,{"id":43,"source_url":44,"license_code":35,"credit_html":45,"title":46,"description":38,"author":39,"original_width":47,"original_height":48},55676,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=84622243","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=84622243\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Framesite diamondite (South Africa) 4 (49169490423).jpg",1414,1375,{"id":50,"source_url":51,"license_code":35,"credit_html":52,"title":53,"description":38,"author":39,"original_width":54,"original_height":55},55677,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=84622244","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=84622244\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Framesite diamondite (South Africa) 3 (49169490543).jpg",1922,1397,{"id":57,"source_url":58,"license_code":35,"credit_html":59,"title":60,"description":38,"author":39,"original_width":61,"original_height":62},55678,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=84622246","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=84622246\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Framesite diamondite (South Africa) 2 (49169490618).jpg",1674,1367,{"id":64,"source_url":65,"license_code":35,"credit_html":66,"title":67,"description":68,"author":39,"original_width":69,"original_height":70},22853,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=97240512","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=97240512\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Framesite diamondite (South Africa) 5.jpg","(65.63 carats)\n\u003Chr>\n\u003Cp>Diamondites are very rare, monomineralic diamond rocks.  \"Diamond\" is the name of a mineral and gemstone.  \"Diamondite\" is a rock name.  Several named varieties of diamondites exist, based on physical characteristics - for example, carbonado, framesite, stewardite (stewartite), and yakutite.\n\u003C\u002Fp>\u003Cp>Seen here is a large framesite diamondite from South Africa.  The specific provenance has not been preserved, but according to the published literature, framesite is often produced from the Premier Mine and the Venetia Mine in South Africa (Heaney et al., 2005).  Other sources of framesite are the Orapa Mine and the Jwaneng Mine in Botswana, southern Africa.\n\u003C\u002Fp>\u003Cp>Framesite is a granular, crystalline-textured diamondite.  Unlike carbonado diamondites (see elsewhere in this photo album), framesite is not cryptocrystalline - the crystals here are much larger.  The rock has a mix of large and small crystals (this would be called porphyritic in a granite).\n\u003C\u002Fp>\u003Cp>Framesites are igneous in origin and occur in kimberlite and lamproite diatremes.  Carbonados are not associated with igneous diatremes - based on isotopic composition, they may be extraterrestrial in origin, possibly supernova rocks.\n\u003C\u002Fp>\u003Cp>Locality: unrecorded\u002Fundisclosed mine in South Africa.\n\u003C\u002Fp>\n\u003Chr>\n\u003Cp>Some framesite references:\n\u003C\u002Fp>\u003Cp>Kurat & Dobosi (2000) - Garnet and diopside-bearing diamondites (framesites).  Mineralogy and Petrology 69: 143-159.\n\u003C\u002Fp>\u003Cp>Heaney et al. (2005) - Strange diamonds: the mysterious origins of carbonado and framesite.  Elements 1: 85-89.\n\u003C\u002Fp>\nTappert & Tappert (2011) - Chapter 2: the morphology of diamonds.  pp. 15-42 in  Diamonds in Nature: a Guide to Rough Diamonds.",1698,1326,{"id":72,"source_url":73,"license_code":35,"credit_html":74,"title":75,"description":68,"author":39,"original_width":76,"original_height":77},22854,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=97240514","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=97240514\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Framesite diamondite (South Africa) 7.jpg",1742,1277,{"id":79,"source_url":80,"license_code":35,"credit_html":81,"title":82,"description":68,"author":39,"original_width":83,"original_height":84},22855,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=97240515","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=97240515\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Framesite diamondite (South Africa) 6.jpg",1945,1626,{"id":86,"source_url":87,"license_code":35,"credit_html":88,"title":89,"description":68,"author":39,"original_width":90,"original_height":91},22856,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=97240516","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=97240516\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Framesite diamondite (South Africa) 8.jpg",1545,1385,[],[],[],{"history":8,"applications":8}]