Amazon Basin (sedimentary basin)

{{Infobox sedimentary basin

| name = Amazon Basin

| other_name = Bacia do Amazonas

| named_for = Amazon River

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| pushpin_map = Brazil

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| map_image = Amazon Basin2.jpg

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| map_caption = The basin is located in the center and center-right of the picture.

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| coordinates = {{coord|2|29|47|S|57|3|25|W|display:inline,title}}

| location = South America

| region = North

| country = {{BRA}}

| state = Amazonas, Pará

| cities = Manaus

| onoffshore = Onshore

| boundaries = Guiana Shield, Gurupá Arch; Marajó Basin, Brazilian Shield, Púrus Arch; Solimões Basin

| partof = Amazon basins

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| rivers = Amazon River

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| area = {{convert|620000|km2|sqmi|abbr=on}}

| basin_type = Continental rift basin

| plate = South America

| orogeny =

| age = Cambrian-recent

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File:Amazon alluvium deposit - autazes.jpg

The Amazon Basin is a large sedimentary basin (620,000 square kilometres (240,000 sq mi)) located near the middle and lower course of the Amazon River, south the Guiana Shield and north of the Central Brazilian Shield. The basin developed on a rift that originated about 550 million years ago during the Cambrian.

Location

The Amazon Basin is located south of the Guiana Shield, north of the Central Brazilian Shield, east of the Solimões Basin, and west of the Marajó Basin. It is bound to the west by the Púrus Arch and in the east by the Gurupá Arch. The basin has an elongated shape with a WSW-ENE orientation. Its long axis runs from the vicinity of Manaus to the area near the confluence of Xingu River with the Amazon River.

Evolution of the basin

The Amazon Basin was developed on a rift, called the Sub-Amazonal Rift, that originated about 550 million years ago during continental collision of the West African Craton.{{cite journal|last1=Burke|first1=Kevin C.|last2=Lytwyn|first2=Jennifer|date=1993|title=Origin of the Rift Under the Amazon Basin as a Result of Continental Collision During Pan-African Time|journal=International Geology Review|volume=35|issue=10|pages=881–897|doi=10.1080/00206819309465563}} Parts of the rift were reactivated during the opening of the South Atlantic. The Amazon Basin evolved through tectonic activity including continental collision, subduction, and distortion of parts of the Andes Mountain Range.{{Cite journal|last1=Latrubesse|first1=Edgardo M.|last2=Cozzuol|first2=Mario|last3=da Silva-Caminha|first3=Silane A. F.|last4=Rigsby|first4=Catherine A.|last5=Absy|first5=Maria Lucia|last6=Jaramillo|first6=Carlos|date=2010|title=The Late Miocene paleogeography of the Amazon Basin and the evolution of the Amazon River system|url=https://www.sciencedirect.com/science/article/pii/S0012825210000140|journal=Earth-Science Reviews|language=en|volume=99|issue=3|pages=99–124|doi=10.1016/j.earscirev.2010.02.005|s2cid=129666624 |issn=0012-8252}}

Bauxite deposits

The Amazon basin hosts large deposits of the aluminum-rich sedimentary rock bauxite. The discovery of bauxite deposits approximately 70 years ago{{Cite journal|last=Grubb|first=P. L. C.|date=1979|title=Genesis of bauxite deposits in the lower Amazon Basin and Guianas coastal plain|url=https://doi.org/10.2113/gsecongeo.74.4.735|journal=Economic Geology|volume=74|issue=4|pages=735–750|doi=10.2113/gsecongeo.74.4.735|issn=0361-0128}} made Brazil one of the most important countries in terms of both production and possession of bauxite deposits.

References

Category:Geology of Brazil

Category:Sedimentary basins of Brazil

Category:Paleozoic rifts and grabens