{"id":2561,"date":"2022-08-01T12:43:03","date_gmt":"2022-08-01T12:43:03","guid":{"rendered":"https:\/\/www.sedimentologia.org.ar\/spa\/?post_type=avada_portfolio&p=2561"},"modified":"2022-08-20T11:59:43","modified_gmt":"2022-08-20T11:59:43","slug":"actinolita","status":"publish","type":"avada_portfolio","link":"https:\/\/www.sedimentologia.org.ar\/spa\/atlas\/actinolita\/","title":{"rendered":"ACTINOLITA"},"content":{"rendered":"
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<\/i>ANTERIOR<\/span><\/a><\/div><\/div><\/div>
SIGUIENTE<\/span><\/i><\/a><\/div><\/div><\/div>

ACTINOLITA (Actinolite)<\/strong><\/h1><\/div>
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Sistema cristalino Monocl\u00ednico
\nGravedad especif. 3 a 3,3
\nAlto relieve (n=1,63).
\nH\u00e1bito prism\u00e1tico, a veces euhedral.
\nForma cristalina, como cristales o agregado fibroso.<\/strong>
\nFractura astillosa. <\/strong>Clivaje perfecto en (110), con intersecciones a 56\u00ba y 124\u00ba, partici\u00f3n en (100).
\nBrillo v\u00edtreo.
\nColor: incoloro, verde claro, verde oscuro, verde gris\u00e1ceo, amarillo.
\nDiafanidad: transparente a translucente.
\nExtinci\u00f3n oblicua de bajo \u00e1ngulo.<\/strong> Pleocro\u00edsmo d\u00e9bil a moderado, de amarillo claro, verde amarillento a verde azulado oscuro p\u00e1lido.
\nBirrefringencia moderada<\/strong> en secciones con espesores de 30 micras. En grano suelto depender\u00e1 del espesor, puede llegar a 0.006. Bi\u00e1xico negativo.
\nUsualmente deriva de rocas del metamorfismo regional de bajo grado o del metamorfismo de contacto de rocas carbon\u00e1ticas magnesianas; tambi\u00e9n de esquistos azules con glauc\u00f3fano.<\/p>\n<\/div><\/div><\/div>

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Clase Strunz: SILICATO – INOSILICATO
\n<\/span><\/strong>Familia de anf\u00edboles
\nSerie actinolita- tremolita- ferro-actinolita
\nCa2(Mg; Fe 2+)5Si8O22(OH)2<\/p>\n<\/div>

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<\/i>https:\/\/www.mindat.org<\/span><\/a><\/div>
<\/i>http:\/\/www.handbookofmineralogy.com<\/span><\/a><\/div><\/div><\/div>
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<\/i>VOLVER AL \u00cdNDICE<\/span><\/a><\/div><\/div><\/div><\/div><\/div>\n","protected":false},"excerpt":{"rendered":"","protected":false},"author":2,"featured_media":2811,"menu_order":0,"comment_status":"open","ping_status":"closed","template":"","format":"standard","meta":{"footnotes":""},"portfolio_category":[26],"portfolio_skills":[],"portfolio_tags":[],"class_list":["post-2561","avada_portfolio","type-avada_portfolio","status-publish","format-standard","has-post-thumbnail","hentry","portfolio_category-minerales"],"_links":{"self":[{"href":"https:\/\/www.sedimentologia.org.ar\/spa\/wp-json\/wp\/v2\/avada_portfolio\/2561","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.sedimentologia.org.ar\/spa\/wp-json\/wp\/v2\/avada_portfolio"}],"about":[{"href":"https:\/\/www.sedimentologia.org.ar\/spa\/wp-json\/wp\/v2\/types\/avada_portfolio"}],"author":[{"embeddable":true,"href":"https:\/\/www.sedimentologia.org.ar\/spa\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/www.sedimentologia.org.ar\/spa\/wp-json\/wp\/v2\/comments?post=2561"}],"version-history":[{"count":59,"href":"https:\/\/www.sedimentologia.org.ar\/spa\/wp-json\/wp\/v2\/avada_portfolio\/2561\/revisions"}],"predecessor-version":[{"id":2890,"href":"https:\/\/www.sedimentologia.org.ar\/spa\/wp-json\/wp\/v2\/avada_portfolio\/2561\/revisions\/2890"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.sedimentologia.org.ar\/spa\/wp-json\/wp\/v2\/media\/2811"}],"wp:attachment":[{"href":"https:\/\/www.sedimentologia.org.ar\/spa\/wp-json\/wp\/v2\/media?parent=2561"}],"wp:term":[{"taxonomy":"portfolio_category","embeddable":true,"href":"https:\/\/www.sedimentologia.org.ar\/spa\/wp-json\/wp\/v2\/portfolio_category?post=2561"},{"taxonomy":"portfolio_skills","embeddable":true,"href":"https:\/\/www.sedimentologia.org.ar\/spa\/wp-json\/wp\/v2\/portfolio_skills?post=2561"},{"taxonomy":"portfolio_tags","embeddable":true,"href":"https:\/\/www.sedimentologia.org.ar\/spa\/wp-json\/wp\/v2\/portfolio_tags?post=2561"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}