A. Marcos

发表

Seismic structure of the northern continental margin of Spain from ESCIN deep seismic profiles

J. A. Pulgar, D. Córdoba, A. Pérez-Estaún, 1996 .

Convergence in a thermally softened thick crust: Variscan intracontinental tectonics in Iberian plate rocks

A. Marcos, S. Llana-Fúnez, 2007 .

The Malpica Lamego Line: a major crustal-scale shear zone in the Variscan belt of Iberia

A. Marcos, S. Llana-Fúnez, 2001 .

Structural record during exhumation and emplacement of high-pressure–low- to intermediate-temperature rocks in the Malpica-Tui unit (Variscan Belt of Iberia)

A. Marcos, S. Llana-Fúnez, 2002 .

Strain geometry in Concepenido eclogites during widespread HP deformation (Cabo Ortegal Complex, NW Spain)

K. Kunze, A. Marcos, S. Llana-Fúnez, 2005 .

Geodynamic evolution of the San Vitero basin, a foreland-type basin developed in the hinterland of the Variscan Orogen (Zamora, NW Spain)

A. Marcos, P. Farias, 2019, Journal of Iberian Geology.

U–Pb evidence for a polyorogenic evolution of the HP–HT units of the NW Iberian Massif

F. J. Fernández, F. Corfu, J. R. Martínez Catalán, 2002 .

An example of low-Th/U zircon overgrowths of magmatic origin in a late orogenic Variscan intrusion: the San Ciprián massif (NW Spain)

F. J. Martinez, J. Aleinikoff, A. Marcos, 2015, Journal of the Geological Society.

The metamorphic evolution of the high pressure mafic granulites of the Bacariza Formation (Cabo Ortegal Complex, Hercynian belt, NW Spain)

A. Marcos, G. Galán, 2000 .

The high-pressure granulites of the Bacariza Formation: an earlier stage in the exhumation of other eclogites in the Cabo Ortegal Complex (Hecynian belt, NW Spain)

A. Marcos, G. Galán, 1999 .

Geochemical evolution of high-pressure mafic granulites from the Bacariza formation (Cabo Ortegal complex, NW Spain): an example of a heterogeneous lower crust

A. Marcos, G. Galán, 1997 .

U–Pb zircon SHRIMP evidence for Cambrian volcanism in the Schistose Domain within the Galicia-Trás-os-Montes Zone (Variscan Orogen, NW Iberian Peninsula)

C. Fanning, A. Marcos, Á. Rubio-Ordoñez, 2014 .

Insights on high-grade deformation in quartzo-feldspathic gneisses during the early Variscan exhumation of the Cabo Ortegal nappe, NW Iberia

F. J. Fernández, A. Marcos, P. Castiñeiras, 2016 .

High-grade deformation in quartzo-feldspathic gneisses during the early Variscan exhumation of the Cabo Ortegal nappe, NW of Iberia

F. J. Fernández, A. Marcos, P. Castiñeiras, 2015 .

Upper ordovician turbidites in western Asturias: A facies analysis with particular reference to vertical and lateral variations

A. Pérez-Estaún, T. Crimes, A. Marcos, 1974 .

The Psammichnites-Taphrhelminthopsis conundrum: Implications for Calibrating the Cambrian explosion

S. Jensen, R. MacNaughton, L. Buatois, 2022, Earth-Science Reviews.

A thin‐skinned tectonics model for an arcuate fold and thrust belt: The Cantabrian Zone (Variscan Ibero‐Armorican Arc)

J. A. Pulgar, J. Marquínez, J. L. Alonso, 1988 .

Trilobite traces and the age of the lowest part of the Ordovician reference section for NW Spain

T. Crimes, A. Marcos, 1976, Geological Magazine.

Mélanges and other types of block-in-matrix formations in the Cantabrian Zone (Variscan Orogen, northwest Spain): origin and significance

J. L. Alonso, L. Fernández, E. Villa, 2015 .

Setting new constrains on the age of crustal-scale extensional shear zone (Vivero fault): implications for the evolution of Variscan orogeny in the Iberian massif

A. Iriondo, A. Marcos, S. Llana-Fúnez, 2015, International Journal of Earth Sciences.

Structure and Organization of the Porma Mélange: Progressive Denudation of a Submarine Nappe Toe by Gravitational Collapse

J. L. Alonso, A. Marcos, Á. Suárez, 2006 .

3-D strain distribution in the Ibero-Armorican arc : a review

F. J. Fernández, H. Chaminé, F. Rosas, 2003 .

Persistent basement wrenching as controlling mechanism of Variscan thin-skinned thrusting and sedimentation, Cantabrian Mountains, Spain: Comment

J. A. Pulgar, J. L. Alonso, A. Marcos, 1991 .

Facies differentiation caused by wrench deformation along a deep-seated fault system (León line, Cantabrian Mountains, North Spain)—discussion

A. Marcos, 1979 .

Superimposed folding under flexural conditions in the Cantabrian Zone (Hercynian Cordillera, northwest Spain)

A. Marcos, M. Julivert, 1973 .

Tectonic framework of the Cabo Ortegal Complex: A slab of lower crust exhumed in the Variscan orogen (northwestern Iberian Peninsula)

F. J. Fernández, A. Marcos, S. Llana-Fúnez, 2002 .

Mylonitic Foliation Developed by Heterogeneous Pure Shear under High-Grade Conditions in Quartzofeldspathic Rocks (Chímparra Gneiss Formation, Cabo Ortegal Complex, NW Spain)

F. J. Fernández, A. Marcos, 1996 .

A U–Pb zircon age (479 ± 5 Ma) from the uppermost layers of the Ollo de Sapo Formation near Viveiro (NW Spain): implications for the duration of rifting-related Cambro-Ordovician volcanism in Iberia

A. Iriondo, A. Marcos, M. Lopez-Sanchez, 2014, Geological Magazine.

Deformation structures and processes within the continental crust: an introduction

F. Bastida, A. Marcos, S. Llana-Fúnez, 2014 .

Crustal structure of the Cantabrian Zone: seismic image of a Variscan foreland thrust and fold belt (NW Spain)

A. Pérez-Estaún, D. Barba, E. Banda, 1995 .

Results from the ESCI-N3.3 marine deep seismic profile along the Cantabrian continental margin

J. A. Pulgar, A. Pérez-Estaún, F. Bastida, 1995 .

Results from the ESCI-N3.1 and ESCI-N3.2 marine deep seismic profiles in the northwestern Galicia Margin

J. A. Pulgar, A. Pérez-Estaún, F. Bastida, 1995 .

Tectonic thinning of a crust slice at high pressure and high temperature by ductile-slab breakoff (Cabo Ortegal Complex, northwest Spain)

F. J. Fernández, A. Marcos, S. Llana-Fúnez, 2004 .