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Pórfidos Cupríferos

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Pórfidos Cupríferos

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Chile

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Pórfidos Cupríferos
 

Pórfidos CupríferosOnline version

Pórfidos Cupríferos

by CATALINA GOMEZ LETELIER
1

Los pórfidos cupríferos se forman en zonas de subducción.

2

La roca hospedante típica es andesítica, diorítica o granodiorítica.

3

La alteración propilítica aparece en el centro del sistema porfírico.

4

La alteración potásica se encuentra en el núcleo del sistema.

5

Las vetas tipo M tienen mena abundante.

6

Las vetas tipo B tienen geometría sinuosa.

7

Las vetas tipo EB contienen biotita temprana.

8

La alteración cálcico-sódica corresponde a las raíces profundas del sistema.

9

El Teniente es el mayor pórfido a cielo abierto del mundo.

10

Los pórfidos se asocian a magmas hidratados ricos en volátiles.

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