[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:11389":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":8,"sigelements":8,"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":14,"strunz10ed2":14,"strunz10ed3":14,"strunz10ed4":8,"dana8ed1":14,"dana8ed2":14,"dana8ed3":14,"dana8ed4":14,"csystem":8,"cclass":8,"spacegroup":8,"spacegroupset":14,"a":14,"b":14,"c":14,"alpha":14,"beta":14,"gamma":14,"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":14,"vhnmax":14,"vhnerror":8,"vhng":8,"vhns":8,"commenthard":8,"dmeas":14,"dmeas2":14,"dcalc":14,"dmeaserror":8,"dcalcerror":8,"commentdense":8,"lustre":8,"lustretype":15,"commentluster":8,"diapheny":8,"streak":8,"colour":16,"commentcolor":8,"colors":17,"streak_colors":8,"luminescence":8,"uv":8,"cleavage":8,"cleavagetype":8,"fracturetype":20,"tenacity":8,"commentbreak":8,"opticaltype":8,"opticalsign":8,"opticalalpha":14,"opticalalpha2":14,"opticalalphaerror":8,"opticalbeta":14,"opticalbeta2":14,"opticalbetaerror":8,"opticalgamma":14,"opticalgamma2":14,"opticalgammaerror":8,"opticalomega":14,"opticalomega2":14,"opticalomegaerror":8,"opticalepsilon":14,"opticalepsilon2":14,"opticalepsilonerror":8,"opticaln":14,"opticaln2":14,"opticalnerror":8,"optical2vcalc":14,"optical2vcalc2":14,"optical2vcalcerror":8,"optical2vmeasured":14,"optical2vmeasured2":14,"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":21,"type_specimen_store":8,"description_short":8,"aboutname":22,"rock_parent":8,"rock_parent2":8,"rock_root":23,"rock_bgs_code":8,"meteoritical_code":8,"updttime":24,"reviewed_at":8,"variety_of":8,"varieties":25,"group_members":26,"associates":27,"confused_with":28,"type_localities":29,"occurrence_total":30,"citations":31,"images":52,"structures":185,"synonyms":186,"language_names":189,"wikidata_qid":8,"texts":190},11389,"1:1:11389:6","a11b0e30-3804-462d-b1de-441a62129401","Indochinite",null,2,"variety",10859,71,false,"0","Vitreous","Black, dark brown",[18,19],"black","brown","Conchoidal,Sub-Conchoidal","Unconsolidated sediments.","Named after the region of occurrence - the former French colonies of Indochina (Vietnam, Laos, Cambodia) plus Thailand and southern China.",0,"2025-08-11 12:14:33",[],[],[],[],[],6,[32,35,39,43,48],{"id":33,"year":8,"html":34,"doi":8},16133227,"doi.org (n.d.) \u003Ca target='_blank' rel='nofollow' href='https:\u002F\u002Fdoi.org\u002F10.1073\u002Fpnas.1920576117'>https:\u002F\u002Fdoi.org\u002F10.1073\u002Fpnas.1920576117\u003C\u002Fa>",{"id":36,"year":37,"html":38,"doi":8},16024036,1962,"Barnes, V E and K Pitakpaivan (1962) ORIGIN OF INDOCHINITE TEKTITES Procedings of NAS 48:947-955",{"id":40,"year":41,"html":42,"doi":8},16133228,2012," Povenmire, H. (2012) Possible Indochinite Tektites found in North Western Canada, 75th Annual Meteoritical Society Meeting https:\u002F\u002Fui.adsabs.harvard.edu\u002Flink_gateway\u002F2012M%26PSA..75.5016P\u002FPUB_PDF",{"id":44,"year":45,"html":46,"doi":47},143562,2018,"Cavosie, Aaron J., Timms, Nicholas E., Erickson, Timmons M., Koeberl, Christian (2018) New clues from Earth’s most elusive impact crater: Evidence of reidite in Australasian tektites from Thailand. \u003Ci>Geology\u003C\u002Fi>,  46 (3) 203-206 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1130\u002Fg39711.1'>doi:10.1130\u002Fg39711.1\u003C\u002Fa>","10.1130\u002Fg39711.1",{"id":49,"year":45,"html":50,"doi":51},409373,"Cavosie, Aaron J. (2018) The Enduring Mystery of Australasian Tektites, in \u003Ci>Terroir: Science Related to Grape and Wine Quality\u003C\u002Fi>. \u003Ci>Elements\u003C\u002Fi>,  14 (3) 212-213 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fgselements.14.3.212'>doi:10.2138\u002Fgselements.14.3.212\u003C\u002Fa>","10.2138\u002Fgselements.14.3.212",[53,63,72,81,91,99,107,115,122,129,136,143,150,157,166,175],{"id":54,"source_url":55,"license_code":56,"credit_html":57,"title":58,"description":59,"author":60,"original_width":61,"original_height":62},60810,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=513304","CC BY-SA 3.0","H. Raab (User:Vesta), via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=513304\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Indochinite.jpg","A typical Indochinite from Korath, Thailand. The specimen weights 69g and is about 53 mm wide.","H. Raab (User:Vesta)",1024,768,{"id":64,"source_url":65,"license_code":66,"credit_html":67,"title":68,"description":7,"author":69,"original_width":70,"original_height":71},60812,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=35599255","CC BY-SA 4.0","Heart Fire Ltd, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=35599255\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Indočinit.jpg","Heart Fire Ltd",1944,2592,{"id":73,"source_url":74,"license_code":66,"credit_html":75,"title":76,"description":77,"author":78,"original_width":79,"original_height":80},60815,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=69334389","Eunostos, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=69334389\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Indochinite (\"pierre sacrée\"), exposition Météorites, Muséum national d'histoire naturelle de Paris.jpg","\"Pierre sacrée\", indochinite. VIIIe siècle après J.-C., Cambodge. Tectite exhumée dans les ruines d'un temple au Cambodge. Le contexte exact de sa découverte est inconnu, mais il est probable qu'elle avait une signification religieuse pour les anciens Khmers. Exposée à Paris à l'occasion de l'exposition \"Météorites\", dans le bâtiment de la grande galerie de l'évolution, au Muséum national d'histoire naturelle de Paris (18 octobre 2017 - 10 juin 2018).","Eunostos",4128,3096,{"id":82,"source_url":83,"license_code":84,"credit_html":85,"title":86,"description":87,"author":88,"original_width":89,"original_height":90},60819,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=86365425","CC BY 2.0","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=86365425\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Indochinite (Pleistocene, 783-803 ka; Australasian Tektite Strewn Field, Guangdong, China) 3.jpg","Indochinite - broken chip from the interior of a specimen from South China. (1.7 centimeters across at its widest)\n\u003Cp>Large & small impacts have affected Earth since its formation 4.55 billion years ago.  Compared with the intensely pitted and cratered Moon, Earth has relatively few preserved impact craters, because they have been destroyed by water & glacial erosion.  Impact events are accompanied by tremendous amounts of heat, resulting in melting of much of the ejected pulverized bedrock at ground zero.  The melted material cools quickly, and falls back to Earth in the form of impact splash glasses (a.k.a. tektites).  Tektites are principally composed of amorphous silica (SiO2).  Broken surfaces show a conchoidal fracture.  Tektites from different impact events are given different names.\n\u003C\u002Fp>\nIndochinites are black-colored, moderately common tektites from southeastern Asia that typically are subspherical to tear-drop shaped to dumb-bell shaped.  They are found throughout the Australasian Tektite Strewn Field (a.k.a. Indochinite Tektite Strewn Field).  This strewn field is huge - it's estimated to extend over 10% of Earth's surface.  Indochinites have been found from Madagascar to Tasmania to South China.  Samples from different geographic areas are often given different names (e.g., australites, thailandites, malaysianites, philippinites, billitonites, vietnamites), but they were all apparently formed by the same event.  The impact crater has never been identified (it's been buried, or eroded away, or the impact event was airburst), but is thought to be in the vicinity of northern Vietnam, based on tetktite abundance patterns.  The age of indochinites has been reported to be about 783 to 803 ka.","James St. John",841,733,{"id":92,"source_url":93,"license_code":84,"credit_html":94,"title":95,"description":96,"author":88,"original_width":97,"original_height":98},60820,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=117480247","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=117480247\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Indochinite tektites (Pleistocene, 783-803 ka; Australasian Tektite Strewn Field, southeastern Asia) 19.jpg","Indochinite tektites from the Pleistocene of southeastern Asia.\n\u003Cp>Large and small impacts have affected Earth since its formation 4.55 billion years ago.  Compared with the intensely pitted and cratered Moon, Earth has relatively few preserved impact craters, because they have been destroyed by water erosion, glacial erosion, and plate tectonics.  Impact events are accompanied by significant heating, which results in melting of much of the ejected pulverized target rocks.  The melted material cools quickly while falling back to Earth and forms tektites - impact splash glasses.  Tektites are principally composed of amorphous silica (SiO2).  Broken surfaces show a conchoidal fracture.  Tektites from different impact events are given different names.\n\u003C\u002Fp>\u003Cp>Indochinites are black-colored tektites from southeastern Asia that typically are subspherical to teardrop-shaped to dumbbell-shaped.  They are found throughout the Australasian Tektite Strewn Field (a.k.a. Indochinite Tektite Strewn Field).  This strewn field is huge - it's estimated to extend 10 to 20% of Earth's surface.  Indochinites have been found from Madagascar to Antarctica to Tasmania to South China.  Samples from different geographic areas are often given different names (e.g., australites, thailandites, malaysianites, philippinites, billitonites, vietnamites), but they were all apparently formed by the same event.  The site of the impact crater has long been a mystery, but has now been identified as likely buried by basaltic lava flows in Laos, southeastern Asia (Sieh et al., 2019).  The age of indochinites has been reported to be about 783 to 803 ka.\n\u003C\u002Fp>\u003Cp>Locality: unrecorded\u002Fundisclosed site in southeastern Asia\n\u003C\u002Fp>\n\u003Chr>\n\u003Cp>Reference cited:\n\u003C\u002Fp>\nSieh et al. (2019) - Australasian impact crater buried under the Bolaven Volcanic Field, southern Laos.  Proceedings of the National Academy of Sciences 117: 1346-1353.",3401,2782,{"id":100,"source_url":101,"license_code":84,"credit_html":102,"title":103,"description":104,"author":88,"original_width":105,"original_height":106},60821,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=117480254","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=117480254\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Indochinite tektite (Pleistocene, 783-803 ka; Australasian Tektite Strewn Field, southeastern Asia) 23.jpg","Indochinite tektite from the Pleistocene of southeastern Asia.\n\u003Cp>Large and small impacts have affected Earth since its formation 4.55 billion years ago.  Compared with the intensely pitted and cratered Moon, Earth has relatively few preserved impact craters, because they have been destroyed by water erosion, glacial erosion, and plate tectonics.  Impact events are accompanied by significant heating, which results in melting of much of the ejected pulverized target rocks.  The melted material cools quickly while falling back to Earth and forms tektites - impact splash glasses.  Tektites are principally composed of amorphous silica (SiO2).  Broken surfaces show a conchoidal fracture.  Tektites from different impact events are given different names.\n\u003C\u002Fp>\u003Cp>Indochinites are black-colored tektites from southeastern Asia that typically are subspherical to teardrop-shaped to dumbbell-shaped.  They are found throughout the Australasian Tektite Strewn Field (a.k.a. Indochinite Tektite Strewn Field).  This strewn field is huge - it's estimated to extend 10 to 20% of Earth's surface.  Indochinites have been found from Madagascar to Antarctica to Tasmania to South China.  Samples from different geographic areas are often given different names (e.g., australites, thailandites, malaysianites, philippinites, billitonites, vietnamites), but they were all apparently formed by the same event.  The site of the impact crater has long been a mystery, but has now been identified as likely buried by basaltic lava flows in Laos, southeastern Asia (Sieh et al., 2019).  The age of indochinites has been reported to be about 783 to 803 ka.\n\u003C\u002Fp>\u003Cp>Locality: unrecorded\u002Fundisclosed site in southeastern Asia\n\u003C\u002Fp>\n\u003Chr>\n\u003Cp>Reference cited:\n\u003C\u002Fp>\nSieh et al. (2019) - Australasian impact crater buried under the Bolaven Volcanic Field, southern Laos.  Proceedings of the National Academy of Sciences 117: 1346-1353.",1286,1434,{"id":108,"source_url":109,"license_code":84,"credit_html":110,"title":111,"description":112,"author":88,"original_width":113,"original_height":114},60822,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=117500348","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=117500348\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Indochinite tektite (Pleistocene, 783-803 ka; Australasian Tektite Strewn Field, southeastern Asia) 25.jpg","Indochinite tektite from the Pleistocene of southeastern Asia, most similar to bellitonite.\n\u003Cp>Large and small impacts have affected Earth since its formation 4.55 billion years ago.  Compared with the intensely pitted and cratered Moon, Earth has relatively few preserved impact craters, because they have been destroyed by water erosion, glacial erosion, and plate tectonics.  Impact events are accompanied by significant heating, which results in melting of much of the ejected pulverized target rocks.  The melted material cools quickly while falling back to Earth and forms tektites - impact splash glasses.  Tektites are principally composed of amorphous silica (SiO2).  Broken surfaces show a conchoidal fracture.  Tektites from different impact events are given different names.\n\u003C\u002Fp>\u003Cp>Indochinites are black-colored tektites from southeastern Asia that typically are subspherical to teardrop-shaped to dumbbell-shaped.  They are found throughout the Australasian Tektite Strewn Field (a.k.a. Indochinite Tektite Strewn Field).  This strewn field is huge - it's estimated to cover 10 to 20% of Earth's surface.  Indochinites are found from Madagascar to Antarctica to Tasmania to South China.  Samples from different geographic areas are often given different names (e.g., australites, thailandites, malaysianites, philippinites, billitonites, vietnamites), but they were all apparently formed by the same event.  The site of the impact crater has long been a mystery, but is now identified as likely buried by basaltic lava flows in Laos, southeastern Asia (Sieh et al., 2019).  The age of indochinites is about 783 to 803 ka.\n\u003C\u002Fp>\u003Cp>Locality: unrecorded\u002Fundisclosed site in southeastern Asia\n\u003C\u002Fp>\n\u003Chr>\n\u003Cp>Reference cited:\n\u003C\u002Fp>\nSieh et al. (2019) - Australasian impact crater buried under the Bolaven Volcanic Field, southern Laos.  Proceedings of the National Academy of Sciences 117: 1346-1353.",1685,1226,{"id":116,"source_url":117,"license_code":84,"credit_html":118,"title":119,"description":120,"author":88,"original_width":106,"original_height":121},60823,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=117500352","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=117500352\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Indochinite tektite (Pleistocene, 783-803 ka; Australasian Tektite Strewn Field, southeastern Asia) 26.jpg","Indochinite tektite from the Pleistocene of southeastern Asia.\n\u003Cp>Large and small impacts have affected Earth since its formation 4.55 billion years ago.  Compared with the intensely pitted and cratered Moon, Earth has relatively few preserved impact craters, because they have been destroyed by water erosion, glacial erosion, and plate tectonics.  Impact events are accompanied by significant heating, which results in melting of much of the ejected pulverized target rocks.  The melted material cools quickly while falling back to Earth and forms tektites - impact splash glasses.  Tektites are principally composed of amorphous silica (SiO2).  Broken surfaces show a conchoidal fracture.  Tektites from different impact events are given different names.\n\u003C\u002Fp>\u003Cp>Indochinites are black-colored tektites from southeastern Asia that typically are subspherical to teardrop-shaped to dumbbell-shaped.  They are found throughout the Australasian Tektite Strewn Field (a.k.a. Indochinite Tektite Strewn Field).  This strewn field is huge - it's estimated to cover 10 to 20% of Earth's surface.  Indochinites are found from Madagascar to Antarctica to Tasmania to South China.  Samples from different geographic areas are often given different names (e.g., australites, thailandites, malaysianites, philippinites, billitonites, vietnamites), but they were all apparently formed by the same event.  The site of the impact crater has long been a mystery, but is now identified as likely buried by basaltic lava flows in Laos, southeastern Asia (Sieh et al., 2019).  The age of indochinites is about 783 to 803 ka.\n\u003C\u002Fp>\u003Cp>Locality: unrecorded\u002Fundisclosed site in southeastern Asia\n\u003C\u002Fp>\n\u003Chr>\n\u003Cp>Reference cited:\n\u003C\u002Fp>\nSieh et al. (2019) - Australasian impact crater buried under the Bolaven Volcanic Field, southern Laos.  Proceedings of the National Academy of Sciences 117: 1346-1353.",1050,{"id":123,"source_url":124,"license_code":84,"credit_html":125,"title":126,"description":120,"author":88,"original_width":127,"original_height":128},60824,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=117500353","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=117500353\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Indochinite tektite (Pleistocene, 783-803 ka; Australasian Tektite Strewn Field, southeastern Asia) 27.jpg",1392,1336,{"id":130,"source_url":131,"license_code":84,"credit_html":132,"title":133,"description":120,"author":88,"original_width":134,"original_height":135},60825,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=117500395","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=117500395\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Indochinite tektite (Pleistocene, 783-803 ka; Australasian Tektite Strewn Field, southeastern Asia) 34.jpg",1722,1289,{"id":137,"source_url":138,"license_code":84,"credit_html":139,"title":140,"description":120,"author":88,"original_width":141,"original_height":142},60826,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=117500397","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=117500397\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Indochinite tektite (Pleistocene, 783-803 ka; Australasian Tektite Strewn Field, southeastern Asia) 35.jpg",1194,1240,{"id":144,"source_url":145,"license_code":84,"credit_html":146,"title":147,"description":120,"author":88,"original_width":148,"original_height":149},60827,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=117500398","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=117500398\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Indochinite tektite (Pleistocene, 783-803 ka; Australasian Tektite Strewn Field, southeastern Asia) 36.jpg",1651,1119,{"id":151,"source_url":152,"license_code":84,"credit_html":153,"title":154,"description":120,"author":88,"original_width":155,"original_height":156},60828,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=117500412","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=117500412\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Indochinite tektite (Pleistocene, 783-803 ka; Australasian Tektite Strewn Field, southeastern Asia) 38.jpg",1222,1055,{"id":158,"source_url":159,"license_code":66,"credit_html":160,"title":161,"description":162,"author":163,"original_width":164,"original_height":165},60829,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=138618897","Geolina163, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=138618897\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Joanneum Naturkundemuseum Indochinit.jpg","Universalmuseum Joanneum Naturkundemuseum: Indochinit","Geolina163",2472,3552,{"id":167,"source_url":168,"license_code":66,"credit_html":169,"title":170,"description":171,"author":172,"original_width":173,"original_height":174},60830,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=147985030","Ladd Observatory, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=147985030\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Muong Nong.jpg","Muong Nong \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FIndochinite\" class=\"extiw\" title=\"w:Indochinite\">Indochinite\u003C\u002Fa>. A layered type of \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002Ftektite\" class=\"extiw\" title=\"w:tektite\">tektite\u003C\u002Fa> found in the \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FUbon_Ratchathani_province\" class=\"extiw\" title=\"w:Ubon Ratchathani province\">Ubon Ratchathani province\u003C\u002Fa> of \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FThailand\" class=\"extiw\" title=\"w:Thailand\">Thailand\u003C\u002Fa>. It has a mass of 56.5 grams.","Ladd Observatory",2660,2032,{"id":176,"source_url":177,"license_code":178,"credit_html":179,"title":180,"description":181,"author":182,"original_width":183,"original_height":184},60818,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=83953759","CC0 1.0","Daderot, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=83953759\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Indochinite, Thailand - University of Arizona Mineral Museum - University of Arizona - Tucson, AZ - DSC08495.jpg","Exhibit in the University of Arizona Mineral Museum - University of Arizona - Tucson, Arizona, USA.","Daderot",3488,4133,[],[187,188],"Indochinit","Indochinita",[],{"history":8,"applications":8}]