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Are subduction zones invading the Atlantic; evidence from the southwest Iberia margin
Are subduction zones invading the Atlantic; evidence from the southwest Iberia margin
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Are subduction zones invading the Atlantic; evidence from the southwest Iberia margin

Duarte, Joao C ; Rosas, Filipe M ; Terrinha, Pedro ; Schellart, Wouter P ; Boutelier, David ; Gutscher, Marc-André ; Ribeiro, Antonio

Geology (Boulder), 2013-08, Vol.41 (8), p.839-842 [Periódico revisado por pares]

Boulder: Geological Society of America (GSA)

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2
Fingerprinting enhanced floodplain reworking during the Paleocene−Eocene Thermal Maximum in the Southern Pyrenees (Spain): Implications for channel dynamics and carbon burial
Fingerprinting enhanced floodplain reworking during the Paleocene−Eocene Thermal Maximum in the Southern Pyrenees (Spain): Implications for channel dynamics and carbon burial
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Fingerprinting enhanced floodplain reworking during the Paleocene−Eocene Thermal Maximum in the Southern Pyrenees (Spain): Implications for channel dynamics and carbon burial

Prieur, Marine ; Whittaker, Alexander C. ; Nuriel, Perach ; Jaimes-Gutierrez, Rocío ; Garzanti, Eduardo ; Roigé, Marta ; Sømme, Tor O. ; Schlunegger, Fritz ; Castelltort, Sébastien

Geology (Boulder), 2024-05 [Periódico revisado por pares]

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3
One or two oroclines in the Variscan Orogen of Iberia? Implications for Pangea amalgamation
One or two oroclines in the Variscan Orogen of Iberia? Implications for Pangea amalgamation
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One or two oroclines in the Variscan Orogen of Iberia? Implications for Pangea amalgamation

Pastor Galan, Daniel ; Groenewegen, Thomas ; Brouwer, Daniel ; Krijgsman, Wout ; Dekkers, Mark J

Geology (Boulder), 2015-06, Vol.43 (6), p.527-530 [Periódico revisado por pares]

Boulder: Geological Society of America (GSA)

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4
Quantifying the post-tectonic topographic evolution of closed basins; the Ebro Basin (northeast Iberia)
Quantifying the post-tectonic topographic evolution of closed basins; the Ebro Basin (northeast Iberia)
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Quantifying the post-tectonic topographic evolution of closed basins; the Ebro Basin (northeast Iberia)

Garcia-Castellanos, Daniel ; Larrasoaña, Juan Cruz

Geology (Boulder), 2015-08, Vol.43 (8), p.663-666 [Periódico revisado por pares]

Boulder: Geological Society of America (GSA)

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5
Zipper junctions; a new approach to the intersections of conjugate strike-slip faults
Zipper junctions; a new approach to the intersections of conjugate strike-slip faults
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Zipper junctions; a new approach to the intersections of conjugate strike-slip faults

Platt, John P ; Passchier, Cees W

Geology (Boulder), 2016-10, Vol.44 (10), p.795-798 [Periódico revisado por pares]

Boulder: Geological Society of America (GSA)

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6
How is topographic simplicity maintained in ephemeral dryland channels?
How is topographic simplicity maintained in ephemeral dryland channels?
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How is topographic simplicity maintained in ephemeral dryland channels?

Singer, Michael Bliss ; Michaelides, Katerina

Geology (Boulder), 2014-12, Vol.42 (12), p.1091-1094 [Periódico revisado por pares]

Boulder: Geological Society of America (GSA)

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7
Small, isolated glacial catchments as priority targets for cosmogenic surface exposure dating of Pleistocene climate fluctuations, southeastern Pyrenees
Small, isolated glacial catchments as priority targets for cosmogenic surface exposure dating of Pleistocene climate fluctuations, southeastern Pyrenees
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Small, isolated glacial catchments as priority targets for cosmogenic surface exposure dating of Pleistocene climate fluctuations, southeastern Pyrenees

Pallàs, Raimon ; Rodés, Ángel ; Braucher, Régis ; Bourlès, Didier L ; Delmas, Magali ; Calvet, Marc ; Gunnell, Yanni

Geology (Boulder), 2010-10, Vol.38 (10), p.891-894 [Periódico revisado por pares]

Boulder: Geological Society of America (GSA)

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8
Normal faulting driven by denudational isostatic rebound
Normal faulting driven by denudational isostatic rebound
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Normal faulting driven by denudational isostatic rebound

Fernández-Ibáñez, Fermín ; Pérez-Peña, José Vicente ; Azor, Antonio ; Soto, Juan I ; Azañón, José Miguel

Geology (Boulder), 2010-07, Vol.38 (7), p.643-646 [Periódico revisado por pares]

Boulder: Geological Society of America (GSA)

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9
Deep deformation pattern from electrical anisotropy in an arched orogen (Betic Cordillera, western Mediterranean)
Deep deformation pattern from electrical anisotropy in an arched orogen (Betic Cordillera, western Mediterranean)
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Deep deformation pattern from electrical anisotropy in an arched orogen (Betic Cordillera, western Mediterranean)

Ruiz-Constán, Ana ; Galindo-Zaldívar, Jesús ; Pedrera, Antonio ; Arzate, Jorge A ; Pous, Jaume ; Anahnah, Farida ; Heise, Wiebke ; Monteiro Santos, Fernando A ; Marín-Lechado, Carlos

Geology (Boulder), 2010-08, Vol.38 (8), p.731-734 [Periódico revisado por pares]

Boulder: Geological Society of America (GSA)

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10
Karstification without carbonic acid; bedrock dissolution by gypsum-driven dedolomitization
Karstification without carbonic acid; bedrock dissolution by gypsum-driven dedolomitization
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Karstification without carbonic acid; bedrock dissolution by gypsum-driven dedolomitization

Bischoff, James L ; Julià, Ramon ; Shanks, III ; Rosenbauer, Robert J

Geology (Boulder), 1994-11, Vol.22 (11), p.995-998 [Periódico revisado por pares]

Boulder: Geological Society of America (GSA)

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