The Siderian-Orosirian magmatism in the Gavião Paleoplate, Brazil: U-Pb geochronology, geochemistry and tectonic implications
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- 作者：Simone Cerqueira Pereira Cruza ; simonecruzufba@gmail.com" class="auth_mail" title="E-mail the corresponding author ; Johildo Salomã ; o Figueiredo Barbosaa ; johildo@cpgg.ufba.br" class="auth_mail" title="E-mail the corresponding author ; Marilda Santos Pintob ; mspinto@atarde.com.br" class="auth_mail" title="E-mail the corresponding author ; Jean-Jacques Peucatc ; peucat@univ-rennes1.fr" class="auth_mail" title="E-mail the corresponding author ; Jean Louis Paquetted ; paquette@opgc.univ-bpclermont.fr" class="auth_mail" title="E-mail the corresponding author ; Jailma Santos de Souzaa ; jailmasouza@gmail.com" class="auth_mail" title="E-mail the corresponding author ; Violeta de Souza Martinse ; violeta.martins@cprm.gov.br" class="auth_mail" title="E-mail the corresponding author ; Farid Chemale Jú ; niorf ; fchemale@unb.br" class="auth_mail" title="E-mail the corresponding author ; Mauricio Antonio Carneirog ; mauricio@degeo.ufop.br" class="auth_mail" title="E-mail the corresponding author
- 关键词：Granitoids ; Siderian-Orosirian ; Gaviã ; o Paleoplate ; Sã ; o Francisco Craton
- 刊名：Journal of South American Earth Sciences
- 出版年：2016
- 出版时间：August 2016
- 年：2016
- 卷：69
- 期：Complete
- 页码：43-79
- 全文大小：9171 K
文摘
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Twenty-nine Siderian-Rhyacian-Orosirian granitoids were recognized in the southern Gavião Paleoplate.
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In Gavião Paleoplate the age of Ryacian-Orosirian magmatism ranges between 1944 ± 7 and 2140 ± 9 Ma.
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Data suggest that some rocks were generated in subduction environment.