Articles | Volume 5, issue 2
https://doi.org/10.5194/se-5-1223-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/se-5-1223-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
03 Dec 2014
Research article |
| 03 Dec 2014
Thermal conditions during deformation of partially molten crust from TitaniQ geothermometry: rheological implications for the anatectic domain of the Araçuaí belt, eastern Brazil
G. C. G. Cavalcante
CORRESPONDING AUTHOR
Instituto de Geociências, Universidade de São Paulo, Rua do Lago, 562, 05508-080, São Paulo, Brazil
Géosciences Montpellier, Université de Montpellier 2 & CNRS Place E. Bataillon, 34095 Montpellier Cedex 05, France
A. Vauchez
Géosciences Montpellier, Université de Montpellier 2 & CNRS Place E. Bataillon, 34095 Montpellier Cedex 05, France
C. Merlet
Géosciences Montpellier, Université de Montpellier 2 & CNRS Place E. Bataillon, 34095 Montpellier Cedex 05, France
M. Egydio-Silva
Instituto de Geociências, Universidade de São Paulo, Rua do Lago, 562, 05508-080, São Paulo, Brazil
M. H. Bezerra de Holanda
Instituto de Geociências, Universidade de São Paulo, Rua do Lago, 562, 05508-080, São Paulo, Brazil
B. Boyer
Géosciences Montpellier, Université de Montpellier 2 & CNRS Place E. Bataillon, 34095 Montpellier Cedex 05, France
Viewed
Total article views: 3,804 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 28 May 2014)
| HTML | XML | Total | BibTeX | EndNote | |
|---|---|---|---|---|---|
| 1,409 | 2,213 | 182 | 3,804 | 202 | 209 |
- HTML: 1,409
- PDF: 2,213
- XML: 182
- Total: 3,804
- BibTeX: 202
- EndNote: 209
Total article views: 3,205 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 03 Dec 2014)
| HTML | XML | Total | BibTeX | EndNote | |
|---|---|---|---|---|---|
| 1,116 | 1,932 | 157 | 3,205 | 187 | 198 |
- HTML: 1,116
- PDF: 1,932
- XML: 157
- Total: 3,205
- BibTeX: 187
- EndNote: 198
Total article views: 599 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 28 May 2014)
| HTML | XML | Total | BibTeX | EndNote | |
|---|---|---|---|---|---|
| 293 | 281 | 25 | 599 | 15 | 11 |
- HTML: 293
- PDF: 281
- XML: 25
- Total: 599
- BibTeX: 15
- EndNote: 11
Cited
17 citations as recorded by crossref.
- Adamastor – an ocean that never existed? J. Konopásek et al. 10.1016/j.earscirev.2020.103201
- Connecting the Araçuaí and Ribeira belts (SE – Brazil): Progressive transition from contractional to transpressive strain regime during the Brasiliano orogeny M. Egydio-Silva et al. 10.1016/j.jsames.2018.06.005
- Reconstructing the metamorphic evolution of the Araçuaí orogen (SE Brazil) using in situ U–Pb garnet dating and P–T modelling M. Schannor et al. 10.1111/jmg.12605
- A critical discussion of the subduction-collision model for the Neoproterozoic Araçuaí-West Congo orogen H. Fossen et al. 10.1016/j.precamres.2020.105715
- The role of deformation-assisted by water influx on partial melting of a granite protolith, and its role in the evolution of southwestern São Francisco Craton margin, Brazil E. Julião et al. 10.1016/j.jsames.2021.103605
- Petrologic and geochronological constraints on the polymetamorphic evolution of the collisional granites, Araçuaí Orogen (SE Brazil) S. MAURI et al. 10.1590/0001-3765202120200639
- How long can the middle crust remain partially molten during orogeny? C. Cavalcante et al. 10.1130/G45126.1
- The influence of partial melting and melt migration on the rheology of the continental crust G. Cavalcante et al. 10.1016/j.jog.2016.06.002
- Slow cooling and crystallization of the roots of the Neoproterozoic Araçuaí hot orogen (SE Brazil): Implications for rheology, strain distribution, and deformation analysis A. Vauchez et al. 10.1016/j.tecto.2019.05.013
- Reviewing the puzzling intracontinental termination of the Araçuaí-West Congo orogenic belt and its implications for orogenic development C. Cavalcante et al. 10.1016/j.precamres.2018.12.025
- Temperature and timing of ductile deformation of the Longquanguan shear zone, Trans-North China Orogen J. Liu et al. 10.1016/j.precamres.2021.106217
- The role of Ediacaran synkinematic anatectic rocks and the late-orogenic charnockitic rocks in the development of the hot Araçuaí belt C. Cavalcante et al. 10.1016/j.precamres.2021.106396
- Hot Versus Cold Orogenic Behavior: Comparing the Araçuaí‐West Congo and the Caledonian Orogens H. Fossen et al. 10.1002/2017TC004743
- Building an inversely zoned post-orogenic intrusion in the Neoproterozoic-Cambrian Araçuaí orogen (Brazil) U. Bellon et al. 10.1016/j.jsg.2021.104401
- Temperature constraints on microfabric patterns in quartzofeldsphatic mylonites, Ribeira belt (SE Brazil) C. Cavalcante et al. 10.1016/j.jsg.2018.07.013
- Midcrust deformation regime variations across the Neoproterozoic Araçuaí hot orogen (SE Brazil): Insights from structural and magnetic fabric analyses T. Angelo et al. 10.1016/j.jsg.2020.104007
- Magnetic Fabric and Geochronology of a Cambrian “Isotropic” Pluton in the Neoproterozoic Araçuaí Orogen F. Temporim et al. 10.1029/2019TC005877
17 citations as recorded by crossref.
- Adamastor – an ocean that never existed? J. Konopásek et al. 10.1016/j.earscirev.2020.103201
- Connecting the Araçuaí and Ribeira belts (SE – Brazil): Progressive transition from contractional to transpressive strain regime during the Brasiliano orogeny M. Egydio-Silva et al. 10.1016/j.jsames.2018.06.005
- Reconstructing the metamorphic evolution of the Araçuaí orogen (SE Brazil) using in situ U–Pb garnet dating and P–T modelling M. Schannor et al. 10.1111/jmg.12605
- A critical discussion of the subduction-collision model for the Neoproterozoic Araçuaí-West Congo orogen H. Fossen et al. 10.1016/j.precamres.2020.105715
- The role of deformation-assisted by water influx on partial melting of a granite protolith, and its role in the evolution of southwestern São Francisco Craton margin, Brazil E. Julião et al. 10.1016/j.jsames.2021.103605
- Petrologic and geochronological constraints on the polymetamorphic evolution of the collisional granites, Araçuaí Orogen (SE Brazil) S. MAURI et al. 10.1590/0001-3765202120200639
- How long can the middle crust remain partially molten during orogeny? C. Cavalcante et al. 10.1130/G45126.1
- The influence of partial melting and melt migration on the rheology of the continental crust G. Cavalcante et al. 10.1016/j.jog.2016.06.002
- Slow cooling and crystallization of the roots of the Neoproterozoic Araçuaí hot orogen (SE Brazil): Implications for rheology, strain distribution, and deformation analysis A. Vauchez et al. 10.1016/j.tecto.2019.05.013
- Reviewing the puzzling intracontinental termination of the Araçuaí-West Congo orogenic belt and its implications for orogenic development C. Cavalcante et al. 10.1016/j.precamres.2018.12.025
- Temperature and timing of ductile deformation of the Longquanguan shear zone, Trans-North China Orogen J. Liu et al. 10.1016/j.precamres.2021.106217
- The role of Ediacaran synkinematic anatectic rocks and the late-orogenic charnockitic rocks in the development of the hot Araçuaí belt C. Cavalcante et al. 10.1016/j.precamres.2021.106396
- Hot Versus Cold Orogenic Behavior: Comparing the Araçuaí‐West Congo and the Caledonian Orogens H. Fossen et al. 10.1002/2017TC004743
- Building an inversely zoned post-orogenic intrusion in the Neoproterozoic-Cambrian Araçuaí orogen (Brazil) U. Bellon et al. 10.1016/j.jsg.2021.104401
- Temperature constraints on microfabric patterns in quartzofeldsphatic mylonites, Ribeira belt (SE Brazil) C. Cavalcante et al. 10.1016/j.jsg.2018.07.013
- Midcrust deformation regime variations across the Neoproterozoic Araçuaí hot orogen (SE Brazil): Insights from structural and magnetic fabric analyses T. Angelo et al. 10.1016/j.jsg.2020.104007
- Magnetic Fabric and Geochronology of a Cambrian “Isotropic” Pluton in the Neoproterozoic Araçuaí Orogen F. Temporim et al. 10.1029/2019TC005877
Saved (final revised paper)
Saved (preprint)
Latest update: 14 Jul 2025
