The Santos Formation ( pt, Formacão Santos) is a
geological formation
A geological formation, or simply formation, is a body of rock having a consistent set of physical characteristics (lithology) that distinguishes it from adjacent bodies of rock, and which occupies a particular position in the layers of rock expo ...
of the
Santos Basin
The Santos Basin ( pt, Bacia de Santos) is an approximately large mostly offshore sedimentary basin. It is located in the south Atlantic Ocean, some southeast of Santos, Brazil. The basin is one of the Brazilian basins to have resulted from th ...
offshore of the
Brazil
Brazil ( pt, Brasil; ), officially the Federative Republic of Brazil (Portuguese: ), is the largest country in both South America and Latin America. At and with over 217 million people, Brazil is the world's fifth-largest country by area ...
ian states of
Rio de Janeiro
Rio de Janeiro ( , , ; literally 'River of January'), or simply Rio, is the capital of the Rio de Janeiro (state), state of the same name, Brazil's List of Brazilian states by population, third-most populous state, and the List of largest citi ...
,
São Paulo
São Paulo (, ; Portuguese for 'Saint Paul') is the most populous city in Brazil, and is the capital of the state of São Paulo, the most populous and wealthiest Brazilian state, located in the country's Southeast Region. Listed by the Ga ...
,
Paraná and
Santa Catarina. The predominantly
conglomeratic sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks.
Most sandstone is composed of quartz or feldspar (both silicates ...
formation with interbedded
shale
Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4) and tiny fragments (silt-sized particles) of other minerals, especia ...
s dates to the
Late Cretaceous
The Late Cretaceous (100.5–66 Ma) is the younger of two epochs into which the Cretaceous Period is divided in the geologic time scale. Rock strata from this epoch form the Upper Cretaceous Series. The Cretaceous is named after ''creta'', ...
period;
Cenomanian-
Maastrichtian
The Maastrichtian () is, in the ICS geologic timescale, the latest age (uppermost stage) of the Late Cretaceous Epoch or Upper Cretaceous Series, the Cretaceous Period or System, and of the Mesozoic Era or Erathem. It spanned the interv ...
epochs and has a maximum thickness of .
Etymology
The formation is as the Santos Basin named after the city of
Santos, São Paulo.
Description
The Santos Formation is thick,
[Kiang Chang et al., 2008, p.32] and consists of reddish
lithic conglomerates and
sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks.
Most sandstone is composed of quartz or feldspar (both silicates ...
s, interbedded with grey
shale
Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4) and tiny fragments (silt-sized particles) of other minerals, especia ...
s and reddish clays. These facies are interbedded and change laterally into the
Itajai-Açu and
Juréia Formations. The
depositional environment
In geology, depositional environment or sedimentary environment describes the combination of physical, chemical, and biological processes associated with the deposition of a particular type of sediment and, therefore, the rock types that will b ...
is thought to be transitional continental to marginal marine, ranging from
alluvial
Alluvium (from Latin ''alluvius'', from ''alluere'' 'to wash against') is loose clay, silt, sand, or gravel that has been deposited by running water in a stream bed, on a floodplain, in an alluvial fan or beach, or in similar settings. Al ...
to
braided river
A braided river, or braided channel, consists of a network of river channels separated by small, often temporary, islands called braid bars or, in English usage, '' aits'' or ''eyots''.
Braided streams tend to occur in rivers with high sedime ...
s and deltas. Biostratigraphic data indicate a
Late Cretaceous
The Late Cretaceous (100.5–66 Ma) is the younger of two epochs into which the Cretaceous Period is divided in the geologic time scale. Rock strata from this epoch form the Upper Cretaceous Series. The Cretaceous is named after ''creta'', ...
age (
Cenomanian-
Maastrichtian
The Maastrichtian () is, in the ICS geologic timescale, the latest age (uppermost stage) of the Late Cretaceous Epoch or Upper Cretaceous Series, the Cretaceous Period or System, and of the Mesozoic Era or Erathem. It spanned the interv ...
).
[Clemente, 2013, p.23]
See also
*
Campos Basin
The Campos Basin is one of 12 coastal sedimentary basins of Brazil. It spans both onshore and offshore parts of the South Atlantic with the onshore part located near Rio de Janeiro. The basin originated in Neocomian stage of the Cretaceous perio ...
References
Bibliography
*
* {{cite LSA , last=Kiang Chang , first=Hung , last2=Assine , first2=Mario Luis , last3=Santos Corrêa , first3=Fernando , last4=Setsuo Tinen , first4=Julio , last5=Campane Vidal , first5=Alexandre , last6=Koike , first6=Luzia , year=2008 , title=Sistemas petrolíferos e modelos de acumulação de hidrocarbonetos na Bacia de Santos , url=http://geomuseu.ist.utl.pt/GSP2012/GSP2009/Casos%20de%20estudo%20SP/GSP%20Bacia%20Santos.pdf , journal=
Revista Brasileira de Geociências , volume=38 , pages=29–46 , accessdate=2017-09-04
Geologic formations of Brazil
Santos Basin
Cretaceous Brazil
Upper Cretaceous Series of South America
Maastrichtian Stage of South America
Campanian Stage
Santonian Stage
Coniacian Stage
Turonian Stage
Cenomanian Stage
Conglomerate formations
Sandstone formations
Shale formations
Alluvial deposits
Fluvial deposits
Deltaic deposits
Formations
Formations
Formations
Formations