sedimentary breccia oor Spaans
sedimentary breccia
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Sedimentary breccias are an integral host rock for many sedimentary exhalative deposits.
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Sedimentary breccias are a type of clastic sedimentary rock which are composed of angular to subangular, randomly oriented clasts of other sedimentary rocks.
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In the field, it may at times be difficult to distinguish between a debris flow sedimentary breccia and a colluvial breccia, especially if one is working entirely from drilling information.
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Technically, turbidites are a form of debris flow deposit and are a fine-grained peripheral deposit to a sedimentary breccia flow. as angular, poorly sorted, very immature fragments of rocks in a finer grained groundmass which are produced by mass wasting.
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The Ayawilca deposit consists of Zn-Pb-Cu massive sulfides and some values of Ag in a constant horizon of sedimentary breccias that lie beneath the sands of the Goyllarisquizga formation.
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There it was buried in a detrital sedimentary rock called breccia, a natural cement.
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The deposit is formed by 6 different types of hummocks, according to their compositions: lavic, pyroclastic, sedimentary, mixed, pyroclastic breccia and basaltic-andesitic hummocks.
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Later, during the Devonian – Carboniferous ages, the onset of the subduction generated the accretionary complex (i.e. EAMC) and, therefore, compressional deformative episodes, mainly of ductile type. The Arroyo La Mina Formation is a 50 m thickness succession, which is composed by sedimentary breccias and they overlain to the EAMC by a fault contact. Also, this Formation is overlain by the Ibáñez Formation, which is composed by tuffs, mainly, and it has a 90 m thickness at the study zone.
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Iza volcanic structure (5°36'20''N - 72°59'33'' W) is the result of rising riodacitic to ryolithic magmatic pulses, which didn ́t reach the surface, the first of them giving origin to an intrusive breccias, interpreted as the result of indirect hot deep magma interaction with a sedimentary aquifer, leading to vapor overpressure and consequent fragmentation of the host rocks.
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A breccia is a clastic sedimentary rock composed of angular clasts in a consolidated matrix.
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The intrusive breccia form the Southern part of the Iza edifice, it is massive beige to light red in color, locally with pseudo columnar joint; it is composed by angular to subrounded sedimentary and minor igneous rock fragments in a porphyry rhyotlitic matrix.
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We'll come across phonolitic lavas, Roque Nublo volcanic breccias, basaltic flows, sedimentary deposits and colluvia, as well as freestanding outcrops such as Roque Saucillo or Roque Jincado, made up of hauynite phonolites.
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Tuffs and tuff breccias occur practically all over Georgia in igneous-sedimentary Mid-Jurassic and Upper Cretaceous.
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SUMMARY: In San Pedro de Antromero beach (Asturias) you can see an excellent exhibition of a turbidite (Formation Olleros) where you can see almost all the typical elements of these facies (intervals Bouma, intraformational breccias, landslides, structures sedimentary etc...).
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The host rock is present as breccia fragments of entirely silica-replaced sedimentary rocks from the Cretaceous basement sequence, which crops out just to the south.
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Based on the predominant hummock type and the spatial distribution, the deposit has been divided into 6 different facies (Toreva Block Facies, Volcanic Hummocks Facies, Central Facies, Sedimentary Hummocks Facies, Mixed Facies and Pyroclastic Breccia Hummocks Facies).
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3D modelling of all underground workings, drill holes and surface pits; grade for Au g/t, Ag g/t, Hg ppb and any other metals proven to be useful; the Somera Tuff unconformity; the strike and dip of known veins and vein segments; the known high- and low-angle faults; known alteration boundaries; unique sedimentary horizons that may be more amenable to mineralization (coarser grained or more calcareous) or due to competency contrasts with an objective to gain an understanding of all grade controls including: structural, breccia-hosted, lithology controlled and intensely leached portions of the vein.
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