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h5. Mafic-plutonic sand, Antofagasta,

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Location:

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North Chile, end of road along coast approx. 10 km south of Antofagasta

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Provenance:

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Gabbroid rocks on western slope of the Cerro Coloso

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Composition:

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White plagioclase, black hornblende, absence of quartz

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Texture:

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Coarse sand, poorly sorted, almost not transported detritus

Sample number

Collector

Date of sampling

heubeck0128 - SA16

Christoph Heubeck, Institut für Geologische Wissenschaften, FU Berlin

2005

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Comments:

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 Chile

| !scen.jpg|thumbnail! | | !makro.jpg|thumbnail! |
| Sample area \\
{table-cell:width=30%}
{table-cell} | Macro |

| *Location* \\ | North Chile, end of road along coast approx. 10 km south of Antofagasta |
| *Depositional facies* \\ | _replace this with text about the dep facies_ |
| *Provenance* \\ | Gabbroid rocks on western slope of the Cerro Coloso |
| *Composition* \\ | White plagioclase, black hornblende, absence of quartz |
| *Texture* | Coarse sand, poorly sorted, almost not transported detritus |
h6. Petrographic thin section:
| *Description* | _insert here short description of thin section_ |

| _insert here a bright field image_ |  | _insert here a dark field image_ |
| Bright field {table-cell:width=30%}
{table-cell}| Dark field  |



| *Sample number* | heubeck0128 - SA16 |
| *Collector* | Christoph Heubeck, Institut für Geologische Wissenschaften, FU Berlin | 
| *Date of sampling* | 2005 |




h6. Comments:

The Cerro Coloso is a "core complex" of mafic, plutonic rocks. They are found at > 1000 m on top of the cliff. The slope is described as an "angle of repose" and is covered by salt incrusted gravel and dune sands

[Additional data page|geowisssand:0128 Additional data]