1. Identity statement | |
Reference Type | Journal Article |
Site | mtc-m21b.sid.inpe.br |
Holder Code | isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S |
Identifier | 8JMKD3MGP5W34M/3GD3GDR |
Repository | sid.inpe.br/mtc-m21b/2014/05.30.02.20.47 (restricted access) |
Last Update | 2014:07.16.17.24.44 (UTC) administrator |
Metadata Repository | sid.inpe.br/mtc-m21b/2014/05.30.02.20.48 |
Metadata Last Update | 2018:06.04.03.04.12 (UTC) administrator |
DOI | 10.1016/j.catena.2013.11.021 |
ISSN | 0341-8162 |
Label | scopus 2014-05 RossettiCoBeHaPaCaFr:2014:LaQuFl |
Citation Key | RossettiCoBeHaPaCaFr:2014:LaQuFl |
Title | Late Quaternary fluvial terrace evolution in the main southern Amazonian tributary |
Project | CNPq (471483/06-0; 550331/2010-7). |
Year | 2014 |
Access Date | 2024, May 18 |
Type of Work | journal article |
Secondary Type | PRE PI |
Number of Files | 1 |
Size | 8773 KiB |
|
2. Context | |
Author | 1 Rossetti, Dilce de Fátima 2 Cohen, M. C. L. 3 Bertani, Thiago de Castilho 4 Hayakawa, E. H. 5 Paz, J. D. S. 6 Castro, Darcilea F. 7 Friaes, Y. |
Resume Identifier | 1 8JMKD3MGP5W/3C9JGTQ |
Group | 1 DSR-OBT-INPE-MCTI-GOV-BR 2 3 SER-SRE-SPG-INPE-MCTI-GOV-BR |
Affiliation | 1 Instituto Nacional de Pesquisas Espaciais (INPE) 2 Universidade Federal do Pará, Centro de Geociências, Belém, 66075-900 PA, Brazil 3 Instituto Nacional de Pesquisas Espaciais (INPE) 4 Universidade Federal de Alfenas, Instituto de Ciências da Natureza (ICN), Rua Gabriel Monteiro da Silva, 700-Prédio V Centro-Alfenas/MG, Brazil 5 Universidade Federal do Mato Grosso, Instituto de Ciências Exatas e da Terra, Av Fernando Correia, s/n, Cuiabá, 78060-900 MT, Brazil 6 Instituto Nacional de Pesquisas Espaciais (INPE) 7 Universidade Federal do Pará, Centro de Geociências, Belém, 66075-900 PA, Brazil |
Author e-Mail Address | 1 rossetti@dsr.inpe.br 2 mcohen80@hotmail.com 3 thiagob@dsr.inpe.br 4 ericson_geo@yahoo.com.br 5 jackdspaz@yahoo.com.br 6 darcicastro@yahoo.com.br 7 yurifriaes@hotmail.com |
e-Mail Address | marcelo.pazos@inpe.br |
Journal | Catena |
Volume | 116 |
Pages | 19-37 |
Secondary Mark | A1_ENGENHARIAS_I A1_GEOGRAFIA A2_GEOCIÊNCIAS A2_CIÊNCIAS_AGRÁRIAS_I A2_ENGENHARIAS_III A2_SOCIOLOGIA B2_QUÍMICA B2_CIÊNCIAS_BIOLÓGICAS_I B3_ASTRONOMIA_/_FÍSICA C_ZOOTECNIA_/_RECURSOS_PESQUEIROS |
History (UTC) | 2018-06-04 03:04:12 :: administrator -> marcelo.pazos@inpe.br :: 2014 |
|
3. Content and structure | |
Is the master or a copy? | is the master |
Content Stage | completed |
Transferable | 1 |
Content Type | External Contribution |
Version Type | publisher |
Keywords | aggradation deposition fluvial landform lowland environment Quaternary regional climate river system subsidence tectonic evolution tributary Amazonia South America |
Abstract | Late Quaternary sedimentary deposits from Amazonian lowlands are important geological archives for understanding the origin, evolution and controls of the largest fluvial drainage basin on Earth. Climate has been most often claimed as the main factor affecting river evolution in this region. An increasing volume of publications have also highlighted tectonics as a relevant control. This work investigates the late Quaternary evolution of the Madeira River, the biggest southern tributary of the Amazonas Basin and a major waterway in South America, with the goal of discussing the factor with highest potential of influence on its development in space and time. The approach consisted of carrying out a detailed morphological, sedimentological and chronological characterization of terrace deposits. Three terraces were recognized, which record sandy/pebbly channel, muddy channel/oxbow lake, point bar, floodplain, as well as crevasse channel, crevasse splay and levee deposits. The topographically highest terrace T1 formed in the time interval before 43,500 and 31,696-32,913. cal. yrs BP, the intermediate terrace T2 between 25,338-26,056 and 14,129-14,967. cal. yrs BP, and the lowest terrace T3 between 12,881-13,245 and 3158-3367. cal. yrs BP. These terraces are the testimony of successive downcutting and sediment aggradation. Episodes of terrace erosion and deposition cannot be fully accommodated within the framework of fluctuating river base level tied to Late Pleistocene-Holocene global or regional climate fluctuations. Changes in tectonic subsidence rates might have played an important role in the equilibrium state of this particular fluvial system. © 2013 Elsevier B.V. |
Area | SRE |
Arrangement 1 | urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSR > Late Quaternary fluvial... |
Arrangement 2 | urlib.net > BDMCI > Fonds > Produção pgr ATUAIS > SER > Late Quaternary fluvial... |
doc Directory Content | access |
source Directory Content | there are no files |
agreement Directory Content | there are no files |
|
4. Conditions of access and use | |
Language | en |
Target File | 1-s2.0-S0341816213003019-main.pdf |
User Group | administrator marcelo.pazos@inpe.br |
Reader Group | administrator marcelo.pazos@inpe.br |
Visibility | shown |
Archiving Policy | denypublisher denyfinaldraft24 |
Read Permission | deny from all and allow from 150.163 |
Update Permission | not transferred |
|
5. Allied materials | |
Mirror Repository | iconet.com.br/banon/2006/11.26.21.31 |
Next Higher Units | 8JMKD3MGPCW/3ER446E 8JMKD3MGPCW/3F3NU5S |
Citing Item List | sid.inpe.br/bibdigital/2013/10.18.22.34 5 sid.inpe.br/mtc-m21/2012/07.13.14.44.37 2 sid.inpe.br/bibdigital/2013/09.13.21.11 1 |
URL (untrusted data) | http://dx.doi.org/10.1016/j.catena.2013.11.021 |
Dissemination | WEBSCI; PORTALCAPES; SCOPUS. |
Host Collection | sid.inpe.br/mtc-m21b/2013/09.26.14.25.20 |
|
6. Notes | |
Empty Fields | alternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel format isbn lineage mark month nextedition notes number orcid parameterlist parentrepositories previousedition previouslowerunit progress rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype |
|
7. Description control | |
e-Mail (login) | marcelo.pazos@inpe.br |
update | |
|