Cura-Mallín Group

Cura-Mallín Group (Spanish: Grupo Cura-Mallín) is a heterogeneous group of volcano-sedimentary formations of Oligocene-Miocene age, Colhuehuapian to Laventan in the SALMA classification, in south-central Chile and nearby parts of Argentina.[1][2][3] The sediments belonging to the group were deposited in a lacustrine environment and alongside rivers in an intra-arc basin.[1] Southeast of Laguna del Laja Cura-Mallín Group has a thickness of more than 1,800 metres (5,900 ft).[4] The sediments making up the group deposited in an interval between 22 and 8 million years ago.[3]

Cura-Mallín Group
Stratigraphic range: Upper Oligocene–Middle Miocene
Colhuehuapian-Laventan (SALMA)
TypeGeological group
Unit ofCura-Mallín Basin
 Neuquén Basin
Sub-unitsVarious schemes, see text
UnderliesCajón Negro Formation
Trapa Trapa Formation
OverliesCretaceous granitoids
Jurassic sediments
Thickness>1,800 m (5,900 ft)
Lithology
PrimarySandstone, siltstone, shale, breccia, andesite lava
OtherGrainstone
Location
Coordinates37.7°S 71.2°W / -37.7; -71.2
Approximate paleocoordinates38.3°S 66.4°W / -38.3; -66.4
RegionAraucanía & Bío Bío Regions
Neuquén Province
CountryChile
Argentina
Type section
Named forMallín
Cura-Mallín Group is located in Chile
Cura-Mallín Group
Cura-Mallín Group (Chile)

The outcrops of Cura-Mallín Group are found along a north-south elongate area.[4] The group is considered an equivalent of Abanico Formation, either as a southern extension or as a lateral equivalent of that formation.[4]

Stratigraphy and members

Various subdivision schemes have been proposed for the Cura-Mallín unit since the 1980s. In 1983, Niemeyer and Muñoz identified two members; the Río Queuco Member, overlain by the Malla Malla Member. In two publications published in 1995 and 1997, Suárez and Emperan divided Cura-Mallín Formation in two diachronous members: Guapitrío and Río Pedregoso. Utgé et al. (2009) proposed instead a subdivision into an upper Arroyo Pincheira Member and a lower Lumabia Member.[2]

In a 2017 revision the Cura-Mallín, formerly a formation, was redefined as a group given its great variety of lithologies.[3] The Guapitrío, Río Pedregoso members of Suárez and Emperan became formations according to this scheme. In addition the new scheme include the Mitrauquén Formation that overlies both the Guapitrío and Río Pedregoso Formations as a third formation in the group.[3]

Cura-Mallín Basin

A number of geologists consider Cura-Mallín Basin, the sedimentary basin where the formation deposited, an extensional basin that developed on the western fringes of the much larger Neuquén Basin, while others consider it a back-arc basin. In the Upper Miocene the sedimentary basin was inverted.[5] Relative to other nearby sedimentary basins of Miocene and Oligocene age Cura-Mallín Basin has been more researched.[6]

Fossil content

The group contains abundant mammal fossils including bony fishes, birds and mammals such as rodents, marsupials, Mylodontidaes and Notoungulatas.[4]

Group Fossils Notes
MammalsHeteropsomyinae (aff. Acarechimys) sp., Dasyproctidae (aff. Alloiomys) sp., Prolagostomus sp., Caviomorpha indet., Dasypodidae indet., Typotheria indet.
[7]
Paedotherium minor, Acarechimys sp., aff. Alloiomys sp., ?Hegetotherium sp., aff. Incamys sp., Luantus sp., Maruchito sp., Prostichomys sp., Protacaremys sp., cf. Protypotherium sp., Sipalocyon sp., Abderitidae indet., Astrapotheria indet., Astrapotheriidae indet., Caviomorpha indet., Dasypodidae indet., Eocardiidae indet., Hegetotheriinae indet., Interatheriinae indet., Pachyrukhinae indet., Toxodontidae indet., Typotheria indet.
[8][9]
Colpodon antucoensis, Acarechimys sp., Luantus sp., Protacaremys sp., Protypotherium sp., Sipalocyon sp., Echimyidae indet.
[10][11]
FishesNematogenys cuivi
[12]

Economic geology
See also: Geothermal energy in Chile

The proximity of the Cura-Mallín Group to the stratovolcanoes of Tolhuaca and Lonquimay has made it a reservoir of geothermal energy of interest. Of all units the Rucañanco Member of Guapitrio Formation has been judged to have the most promising reservoir potential.[3]

References
  1. Suárez & Emparan, 1995
  2. Utgé et al., 2009
  3. Pedroza et al., 2017
  4. Flynn et al., 2008
  5. Radic, 2010
  6. Franzese et al., 2011
  7. Cerro los Pinos at Fossilworks.org
  8. Trapa Trapa East mid-upper beds at Fossilworks.org
  9. Estero Trapa Trapa West at Fossilworks.org
  10. Shockey et al., 2012
  11. Flynn et al., 2008, p.414
  12. Cerro Rucañanco at Fossilworks.org

Bibliography
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