Active sinking at the bottom of the Rincón de Parangueo Maar (Guanajuato, México) and its probable relation with subsidence faults at Salamanca and Celaya

Abstract Rincon de Parangueo is a Quaternary maar that had a perennial lake until the 1980s. The lake was gradually desiccated as a con - sequence of drawdown in the Salamanca-Valle de Santiago regional aquifer and now functions as a playa-lake. In contrast with the features observed in other crate...

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I whakaputaina i:	Boletín de la Sociedad Geológica Mexicana
Ngā kaituhi matua:	José Jorge Aranda-Gómez, Gilles Levresse, Jesús Pacheco Martínez, José Alfredo Ramos-Leal, Gerardo Carrasco-Núñez, Elizabeth Chacón-Baca, Gildardo González-Naranjo, Gabriel Chávez-Cabello, Marina Vega-González, Gabriel Origel, Cristina Noyola-Medrano
Hōputu:	Artigo
Reo:	Inglês
I whakaputaina:	Sociedad Geológica Mexicana, A.C. 2013
Ngā marau:	Ciencias de la Tierra
Urunga tuihono:	https://www.redalyc.org/articulo.oa?id=94348265014
Ngā Tūtohu:	Tāpirihia he Tūtohu Kāore He Tūtohu, Me noho koe te mea tuatahi ki te tūtohu i tēnei pūkete!