6.- ROCAS IGNEAS, SEDIMENTARIAS, METAMORFICAS.pdf

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6.- ROCAS IGNEAS, SEDIMENTARIAS, METAMORFICAS.pdf

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Ambientes de sedimentación: Los principales macro-ambientes son dos: 1.- Ambiente Ambiente Continen Continental; tal; 2.- Ambien Ambiente te Marino Marino 3.- Ambiente Ambiente Trans Transicion icional al  Sign up to vote on this title Sin embargo existen otros por la gran variabilidad de alt Not useful  Useful de factores: clima, de variedades vegetales y animales y de agentes erosivos.

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Ambiente marino.marino.- Es el ambiente sedimentario más importante sedimentación alcanza el 90 a 95% de la sedimentación total: alg son: · Nerítico.- Es el que se encuentra pegado a la costa cost a desde la or 180 m. b. n. m.; coincide con la zona fótica (con luz) y con la zon oxidación. Sign up to vote on this title

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Not useful · Batial.- Se extiende desde los 180 m.  b. Useful n. m.  hasta los 3800 m

Abisal.- Es el de los fondos marinos por debajo de los 3,800 m

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Rocas sedimentarias clásticas

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CONGLOMERADO.Son rocas formadas por la acumulación y litificación de trozos de otras rocas y/o minerales que tienen como característica común La redondez de dichos


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BRECHAS.- Tienen las mismas características que los Conglomerados,

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diferencia diferencia que sus clastos son angulosos o sub-angulosos sub -angulosos y que ademá sufrieron mayor transporte

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TILLITAS.- Son rocas formadas por la consolidación y diagénesis de mo

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Las morrenas son sedimentos, formados por la erosión glaciaria, depos al final de las masas de hielo; no sufrieron transporte, solo fueron arra

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ARENISCA.- Son rocas formadas de pequeños trozos de minerales o rocas, arrancados de sus lechos, que se acumularon y consolidaron. El tamaño de l componentes componentes de las areniscas cuarzosas o cuarcíferas cuarcíferas oscila entre 2 mm. y 1 Siendo mayoritariamente de cuarzo en porcentajes cercanos cercanos al 90%. El 10% lo compone partículas de feldespatos


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ARCOSA.- Son rocas de grano medio con características características similares a la

cuarzosa y a la Arenisca feldespática; pero con una cantidad de feldesp mayor mayor al 25%. Pueden contener entre 5% y 15% de restos de rocas, de micas; el cemento es de carbonato o de arcilla


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GRAWACKAS.- Se compone de astillas de rocas maficas, de astillas de

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consolidadas y de otras rocas y/o minerales; el cemento es arcilloso. Si rocas son marinas, pertenecen a ambiente reductor.

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LIMOLITAS.- Son rocas compuestas de Limos (1/16 y 1/256 de mm.). El

compone de Cuarzo muy fino, de feldespato microscópico microscópico y de otros mi limo y arcillas


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ARCILLOLITAS.- rocas formadas por la acumulación y petrificación de a

las arcillas, desde el punto de vista sedimentológico, sedimentológico, son partículas men 4 micras: Bauxitas,


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FANGOLITAS FANGOLITAS O LODOLIT LODOLI TAS.-Son rocas compuestas de limo y arcilla en

proporciones diversas, con con características características similares a las Limolitas y Arci

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PIZARRA BLANDA .- Se conoce conoce como como Pizar shale; se presenta en una estructura laminada aún en pequeñas muestras; a diferencia de la roca metamórfica llamada Pizarra (Pizarra slate), no es comp y dura sino quebradiza (no fisible); es diferente a una Lutita Sign up to vote on this title

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LUTITAS.- Es el nombre qu todas las rocas formadas p arcilla o por mezclas de lim en diversas proporciones. L Diferencia Diferencia princip principal al de la Lu demás variedades de rocas de grano fino Sign up to vote on this title

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ROCAS SEDIMENTARIAS NO CLASTICA

rocas sedimentarias que tienen origen acumulación de restos orgánicos o precipitados químicos.

Rocas carbonatadas:  por CALIZA.- Son conformadas Sign rocas up to vote on this title Useful  Not useful minerales carbonatados de origen qu

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TRAVERTINO.- Precipitación química de carbonato de calcio, en forma Aragonito o Calcita, Calcita, a partir de manantiales termales. El Trav Travertino ertino pre estructura "costriforme", irregular, irregular, en forma de columna; textura textura ba masiv masiva a o poro porosa sa


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DOLOMITAS.- Son rocas rocas sedimentar sedimentarias ias no clásticas que contienen más del 50% de Dolomita, también presentan Calcita; en porcentajes muy pequeños contienen Cuarzo, Silex, feldespatos, arcillas, Calcedonia, Hematina, Limonita, Anhidrita, Yeso, Yeso, Halita y otros



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PEDERNAL .- Es una roca roca de sílice que se compone de Calcedonia Calcedonia de gr y/o Cuarzo muy fino, con un porcentaje mayor al 75% de minerales en El Cuarzo puede ser microcristalino microcristalino o criptocristalino,. Las impurezas acompañan a los Chert son: Calcita, Dolomita, Dolomita, Siderita y otros otros (que ca diversa diversa color coloración) ación).. Pedernal, Pedernal, Silex Silex y Chert son sinónimos. sinónimos. Sign up to vote on this title

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DIATOMITAS.- Son acumulaciones de restos restos de diminutas diminutas plantas acuá llamadas diatomeas, que tiene caparazones silíceos de diferentes form bivalvos, de bote, de meda luna, de aguja, de disco. Estas rocas se form agua dulce o marina, de color blanco y de poco peso


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ORGANICAS:

DIATOMITAS.- Son acumulaciones de restos de diminutas plantas acuáticas llamadas diatomeas, que tiene t iene caparazo silíceos de diferentes formas: Sign up to vote on this title

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EVAPORITAS: Los minerales principales que se presentan en la

Evaporitas, son: Halita, Silvita, Celestina, Epsomita, Yeso, Anhidri Ulexita, Colemanita, Borax y otros otros Las Evaporitas son rocas formadas a partir de salmueras (aguas saladas) de origen marino o lacustre Sign up to vote on this title

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HALITA


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YESO


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CARBONES Los carbones minerales, son rocas sedimentarias no clásticas o formadas por la litificación de material vegetal sedimentado con y fragmentos, rocosos o enterrado por ellos.


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TURBA.- Es un carbón en la primera primera fase de formación; se distingue el vegetal vegetal original deshidratado; es de color pardo negruzco, con textur no tiene interés económico ni comercial. LIGNITO.- Es un carbón pardo negruzco, negruzco, de bajo o escaso interés, interés, come debido a su bajo contenido de Carbono. Es muy similar a la turba pero compacto, pese a que conserva su textura leñosa.  HULLA.- Se conoce también también como carbón carbón bituminoso, Sign up to voteporque on this title contiene Useful la Notcombustión; useful adicionalmente grasas de origen orgánico quefacilitan

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6.- ROCAS IGNEAS, SEDIMENTARIAS, METAMORFICAS.pdf

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