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Coquimbo Formation information


Coquimbo Formation
Stratigraphic range: Miocene–Mid Pleistocene
~23–1.2 Ma
PreꞒ
O
S
D
C
P
T
J
K
Pg
N
Marine terrace exposing strata of the Coquimbo Formation, at Caleta Hornos
TypeGeological formation
UnderliesAlluvium
OverliesLiman Formation
Thickness63 m (207 ft)
Lithology
PrimaryConglomerate, sandstone, siltstone, shale and coquina
OtherClay lenses, terra rossa
Location
Coordinates30°20′21″S 71°32′03″W / 30.33917°S 71.53417°W / -30.33917; -71.53417
Approximate paleocoordinates30°06′S 70°18′W / 30.1°S 70.3°W / -30.1; -70.3
RegionCoquimbo Region
CountryCoquimbo Formation Chile
ExtentTongoy Bay
Type section
Named forCoquimbo
Coquimbo Formation is located in Chile
Coquimbo Formation
Coquimbo Formation (Chile)

Coquimbo Formation (Spanish: Formación Coquimbo) is a Miocene to Middle Pleistocene sedimentary formation located in Coquimbo Region in Norte Chico, Chile. The lowermost unit belongs to the lower Miocene, with the third-deepest unit dated at 11.9 ± 1.0 Ma. The uppermost unit of the formation is estimated at 1.2 Ma. In the area of Tongoy, the Coquimbo Formation was deposited in an ancient bay that was formed in a graben or half-graben, with a normal fault dipping east. Sea level changes during the Holocene have caused erosion to cut several marine terraces into the formation.[1]

  1. ^ Le Roux, J.P.; Olivares, Danisa M.; Nielsen, Sven N.; Smith, Norman D.; Middleton, Heather; Fenner, Juliane; Ishman, Scott E. (2006). "Bay sedimentation as controlled by regional crustal behaviour, local tectonics and eustatic sea-level changes: Coquimbo Formation (Miocene–Pliocene), Bay of Tongoy, central Chile" (PDF). Sedimentary Geology. 184 (1–2): 133–153. Bibcode:2006SedG..184..133L. doi:10.1016/j.sedgeo.2005.09.023. Retrieved 11 April 2016.

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