Salta Basin or Salta Rift Basin is a sedimentary basin located in the Argentine Northwest.[1][2] The basin started to accumulate sediments in the Early Cretaceous (Neocomian) and at present it has sedimentary deposits reaching thicknesses of 5,000 metres (16,000 ft). The basin contains seven sub-basins: Tres Cruces, Lomas de Olmedo, Metán, Alemanía, Salfity, El Rey, Sey and Brealito. The basin environment has variously been described as a "foreland rift" and an "intra-continental rift". The basin developed under conditions of extensional tectonics and rift-associated volcanism.[1]
Salta Basin | |
---|---|
Cuenca Salta | |
Location of the basin in Argentina | |
Coordinates | 23°40′S 66°07′W / 23.667°S 66.117°W |
Etymology | Salta Province |
Region | Argentine Northwest |
Country | Argentina Bolivia Chile |
State(s) | Salta, Jujuy, Tucumán Potosí Antofagasta |
Cities | Salta |
Characteristics | |
On/Offshore | Onshore |
Boundaries | Andes |
Part of | Andean foreland basins |
Geology | |
Basin type | Foreland-on-rift basin or intracontinental rift basin |
Plate | South American |
Orogeny | Andean |
Age | Neocomian-Neogene |
Stratigraphy | Stratigraphy |
The basin basement is composed of rocks belonging to the Puncoviscana Formation.[2] The volcanism that began in the Late Jurassic was initially of subalkaline character (low sodium and potassium content), but turned increasingly alkaline in the Early Cretaceous.[1]
The rifts of Salta Basin developed in a time of generalized extensional tectonics along western South America.[3] It has been proposed that the Salar de Atacama depression in Chile was once a westward rift arm of the Salta Basin.[4]
Age | Group | Subgroup | Formation | Lithologies | Basin stage | Notes |
---|---|---|---|---|---|---|
Pliocene | Payogastilla | San Felipe | Conglomerates | Foreland | [5] | |
Huayquerian | Jujuy | Piquete | [6][7] | |||
Huayquerian | Guanaco Sonso | [8] | ||||
Montehermosan | Palo Pintado | [9] | ||||
Chasicoan | ||||||
Laventan | Angastaco | [10][11] | ||||
Friasian | ||||||
Friasian | Metán | Jesús María | [11] | |||
Friasian | Anta | [11] | ||||
Early Miocene | Río Seco | [11] | ||||
Priabonian | Los Colorados | [11] | ||||
Casamayoran | Quebrada de los Colorados | [10] | ||||
Salta | Santa Bárbara | Lumbrera | Late post-rift | [12][13] | ||
Lutetian | ||||||
Itaboraian | Maíz Gordo | [12][14] | ||||
Thanetian | ||||||
Peligran | Mealla | Sandstones, siltstones, conglomerates, paleosols | [12][15] | |||
Selandian | Balbuena | Tunal | Early post-rift | [12] | ||
Danian | Olmedo | [12] | ||||
Yacoraite | Sandstones, limestones | [12] | ||||
Maastrichtian | ||||||
early Maastrichtian | Lecho | Sandstones | [12] | |||
Campanian | Pirgua | Los Blanquitos | Sandstones | Late synrift | [12] | |
Las Curtiembres | Early synrift | [12] | ||||
Santonian | ||||||
Coniacian | ||||||
Turonian | ||||||
Cenomanian | Isonza | Basalt | [12] | |||
Albian | La Yesera | [12] | ||||
Aptian |