The Volcán, a Magmatic Iron Deposit in NW Mexico: Distribution and General Characteristics
The majority of iron deposits in Sonora are associated with skarn zones and/or replacements related to intrusive bodies of granodiorite-quartz monzonite compositions, not greater than 5 Mt and grades less than 50% total Fe. Unlike these deposits, there is the presence of iron deposits whose geologic...
محفوظ في:
| المؤلفون الرئيسيون: | , , |
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| التنسيق: | Online |
| اللغة: | spa |
| منشور في: |
Universida de Sonora
2022
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| الوصول للمادة أونلاين: | https://epistemus.unison.mx/index.php/epistemus/article/view/211 |
| الوسوم: |
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| الملخص: | The majority of iron deposits in Sonora are associated with skarn zones and/or replacements related to intrusive bodies of granodiorite-quartz monzonite compositions, not greater than 5 Mt and grades less than 50% total Fe. Unlike these deposits, there is the presence of iron deposits whose geological characteristics, alteration-mineralization styles and tectonic context, seem to be associated with magmatic processes, which can be classified as IOCG deposits of the iron-apatite type. A typical example of this type is El Volcán, a deposit of ~ 24 Mt of Fe, with an average grade of 40 to 60% Fe. This type of mineral deposit could extend to the western side of Mexico, which represents new opportunities for exploration of this type of deposits. |
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