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1. Identity statement
Reference TypeJournal Article
Sitemtc-m21d.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP3W34T/46M8NUH
Repositorysid.inpe.br/mtc-m21d/2022/04.11.18.43   (restricted access)
Last Update2022:04.11.18.43.20 (UTC) simone
Metadata Repositorysid.inpe.br/mtc-m21d/2022/04.11.18.43.20
Metadata Last Update2023:01.03.16.46.04 (UTC) administrator
DOI10.1016/j.geomorph.2022.108218
ISSN0169-555X
Citation KeyRossettiVaBeVaAlMo:2022:LaDoRe
TitleA large-scale domal relief due to intraplate neotectonic compression in central Amazonia
Year2022
MonthJune
Access Date2024, May 18
Type of Workjournal article
Secondary TypePRE PI
Number of Files1
Size25769 KiB
2. Context
Author1 Rossetti, Dilce de Fátima
2 Vasconcelos, David L.
3 Bezerra, Francisco Hilário R.
4 Valeriano, Márcio de Morisson
5 Alves, Fábio Corrêa
6 Molina, Eder C.
Resume Identifier1 8JMKD3MGP5W/3C9JGTQ
2
3
4 8JMKD3MGP5W/3C9JHPL
Group1 DIOTG-CGCT-INPE-MCTI-GOV-BR
2
3
4 DIOTG-CGCT-INPE-MCTI-GOV-BR
5 DIOTG-CGCT-INPE-MCTI-GOV-BR
Affiliation1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Universidade Federal de Campina Grande (UFCG)
3 Universidade Federal do Rio Grande do Norte (UFRN)
4 Instituto Nacional de Pesquisas Espaciais (INPE)
5 Instituto Nacional de Pesquisas Espaciais (INPE)
6 Universidade de São Paulo (USP)
Author e-Mail Address1 dilce.rossetti@inpe.br
2 davidgeologia2006.1@hotmail.com
3 hilario.bezerra@ufrn.br
4 marcio.valeriano@inpe.br
5 alves.fabioc@gmail.com
6 eder.molina@iag.usp.br
JournalGeomorphology
Volume407
Pagese108218
Secondary MarkA1_INTERDISCIPLINAR A1_GEOGRAFIA A1_GEOCIÊNCIAS A1_ENGENHARIAS_I A1_CIÊNCIAS_AGRÁRIAS_I A2_ENGENHARIAS_III A2_BIODIVERSIDADE B1_CIÊNCIAS_BIOLÓGICAS_I B1_ANTROPOLOGIA_/_ARQUEOLOGIA B2_ASTRONOMIA_/_FÍSICA
History (UTC)2022-04-11 18:43:20 :: simone -> administrator ::
2022-04-11 18:43:21 :: administrator -> simone :: 2022
2022-04-11 18:44:24 :: simone -> administrator :: 2022
2023-01-03 16:46:04 :: administrator -> simone :: 2022
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
KeywordsDomal relief
Growth fold
Intracratonic South America
Neotectonic geomorphology
AbstractIn intracratonic South America, the origin of neotectonic activity and its impact on large Amazonian rivers have been of continuous research interest. Despite the low relief of the land surface, which has generally been attributed to tectonic stability, there is increasing evidence of Neogene fault reactivation within central Amazonia. Recent research has also reported surface folding during the Quaternary, but this record was based only on morphological analysis of remote sensing data. This investigation focuses on a megascale (~60,000 km2) domal relief from central Amazonia (the Juruá dome). It firstly aims to verify the domal relief relationship to folding. It then explores the origin of the stress field from which it has developed within the context of Andean uplift and the westward movement of the South American plate. The approach consisted of analyzing river adjustments based on morphological and morphometric information from remote sensing imagery, integrated with subsurface data Bouguer gravity and magnetic anomaly maps, well logs, and seismic reflection sections. The results revealed that the Juruá dome coincides with the location of a basin depocenter. Subsurface evidence exists for the growth of a broad anticline producing thicker sedimentary units away from the dome core. NE- and NW-striking normal and reverse faults with flower structure geometries are abundant and suggest deformation from strike-slip tectonics. Gravity and magnetic data revealed that the fold and many of its associated faults are deep-rooted into basement rocks. Within the analyzed stratigraphic interval, faults are mostly developed into pre-Cretaceous units, but often propagate to the surface, where they define the edges of the dome and partly deform its overall shape. The fold and its related faults have modified the course of several rivers within the domal relief area, including the Juruá River, which is entrenched along NE-striking faults that are configured to release stress along the fold axis. The geomorphological and structural data are collectively compatible with a long-term NW-trending maximum horizontal compressive stress-field that is driving basin inversion. This neotectonic activity can be linked to far-field stresses from the pushes from the Andean orogeny and the movement of the South American plate against the North Andean and Nazca plates.
AreaSRE
Arrangementurlib.net > BDMCI > Fonds > Produção a partir de 2021 > CGCT > A large-scale domal...
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4. Conditions of access and use
Languageen
Target Filerossetti_2022_large.pdf
User Groupsimone
Reader Groupadministrator
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Visibilityshown
Archiving Policydenypublisher denyfinaldraft24
Read Permissiondeny from all and allow from 150.163
Update Permissionnot transferred
5. Allied materials
Next Higher Units8JMKD3MGPCW/46KUATE
Citing Item Listsid.inpe.br/bibdigital/2022/04.03.22.23 4
sid.inpe.br/mtc-m21/2012/07.13.14.44.37 2
sid.inpe.br/mtc-m21/2012/07.13.14.54.54 1
DisseminationWEBSCI; PORTALCAPES; COMPENDEX; SCOPUS.
Host Collectionurlib.net/www/2021/06.04.03.40
6. Notes
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