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Braided River Sand, Rio Pitai, Santa Cruz, Bolivia

                                                    

Rio Pitai
 

Macro

Location

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Rio Pitai, Santa Cruz, Bolivia

Depositional facies

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Broad, shallow and sandy riverbed

Provenance

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The Rio Pitai drains the Subandean Ranges and erodes thick palaeozoic and mesozoic continental sedimentary rocks as well as thick eolian sediments

Composition

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Quartz

Texture

Medium to fine grained, well sorted, subrounded

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Petrographic thin section:

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Description

Moderately sorted, moderately to well rounded quartz sand. Typical for provenance from a fold belt of clastic sedimentary rocks

 

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Texture:

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Image Added

Bright field

Dark field

Sample number

Heubeck0026

Collector

Christoph Heubeck, Institut für Geologische Wissenschaften, FU Berlin

Date of sampling

 

  2003

 

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Comments:

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Further comments on the sand, depositional history, ecc.The meandering and braided Rio Pitai in the Bolivian lowland of the Amazonas Basin erodes the Subandean Miocene-Recent fold-and -thrust belt. This belt exposes thick continental successions of Carboniferous to Cretaceous eolian sandstones. The supermature source, the high mechanical resistance, and weathering of river sands under a tropical climate all contribute to the maturity. These sands are most likely multiply recycled.

Additional data page