Type Geological formation Other Grainstone | Thickness >1,800 m | |
Sub-units Various schemes, see text Underlies Cajón Negro Formation
Mitrauquén Formation
Trapa Trapa Formation Overlies Cretaceous granitoids
Jurassic sediments Regions Araucanía Region, Bío Bío Region, Neuquén Province Primary Sandstone, Siltstone, Slate, Breccia | ||
Cura-Mallín Formation (Spanish: Formación Cura-Mallín) is a heterogeneous volcano-sedimentary formation of Oligocene-Miocene age in south-central Chile and nearby parts of Argentina. The formation's sediments were deposited in a lake environment and alongide rivers in an intra-arc basin. Southeast of Laguna del Laja Cura-Mallín Formation has a thickness of more than 1,800 m.
Contents
The Cura-Mallín Formation has a north-south elongate form. The formation is considered an equivalent of Abanico Formation, either as a southern extension or as a lateral equivalent of that formation.
The formation contains abundant mammal fossils including Osteichthyan fishes, birds and mammals such as rodents, marsupials, Mylodontidaes and Notoungulatas.
Stratigraphy and members
Various subdivision schemes have been advanced for Cura-Mallín Formation since the 1980s. In 1983 Niemeyer and Muñoz identified two members Río Queuco overlain by Malla Malla. 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.
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. Relative to other nearby sedimentary basins of Miocene and Oligocene age Cura-Mallín Basin has been more researched.