Résumé : Written on recto: "Secretaría de Obras Públicas, Negociado de Calles y Parques. No. 8693, Jun 20-29" Embossed stamp on recto: "Library of Manuel R. Bustamante" (donor). Written on verso: "Frontispiece, Nov. 1930." Probably used by the Munson Steamship Line in their publication, The Cuba Review.
1920-1930
CHC5017
Havana (Cuba)

Droits : http://merrick.library.miami.edu/digitalprojects/copyright.html
chc50170002800001001
1301

Éditeur(s) : London : Printed for John Stockdale London : Printed for John Stockdale
Résumé : Errata: p. [1], following the Preface (i.e., p. xxiv).
A⁴( -A4) b-d⁴ B-2D⁴ 2E² 2F-2I⁴.
The verso of sig. Dd4 is numbered 208-212.
Includes bibliographical references.
This item is part of the West Indies collection.
Has bookplate inside front cover: "Port Elizabeth Public Library, George Owen Smith Collection, 1892".
Spine repaired with leather stamped with gilt; hinges repaired with marbled paper.
Full leather over boards; gilt decorations on covers; marbled endpapers.

Droits : All rights to images are held by the respective holding institution. This image is posted publicly for non-profit educational uses, excluding printed publication. For permission to reproduce images and/or for copyright information contact Special Collections & University Archives, University of Central Florida Libraries, Orlando, FL 32816 phone (407) 823-2576, email: speccoll@mail.ucf.edu
UCF Special Collections Bryant - 5th Floor -- F1923.E26 1797
DP0003441

Résumé : (Ownership) Received by the Rubenstein Library as a gift from Holly Ackerman in 2009. Photographed by Sergio Lastres.
In December 1994, a public monument, called the Liberty Column, was inaugurated in Miami commemorating the journey and suffering of Cuban rafters. Designed by sculptor Enzo Gallo, the statue consists of hands raised to the sky and a round marble column set in a fountain. It is located at Bay Front Park in Miami in front of the Hotel Intercontinental. The statue was vandalized in 2004 and restored by Cuban-American sculptor Marc Andries Smit. The plaque beside the monument reads, “Since 1959, thousands of Cubans have perished anonymously while fleeing tyranny in small boats and makeshift rafts although their names, like martyred refugees of other nations, are written solely on the pages of the sea, this column is a permanent testimony of the human need to be free.”
Cuba
Guantánamo Bay (Cuba)

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
A series of two-stage torsion experiments on Carrara marble were conducted to constrain the influence of known prior deformation on rheological response and microstructural evolution. Comparison with previous experimental data on Carrara marble flow and fabric evolution during single-stage torsion deformation experiments provided direct insights into the significance of initial deformation at various conditions. Our experiments were conducted at 727 degrees C temperature and 300 MPa confining pressure, while maintaining a constant strain rate of 3 x 10(-4) s(-1) on the periphery of the cylindrical samples. Under these conditions, the marble is known to deform in power-law (n = 6-10) ductile flow. All torsion experiments were performed with a Paterson type gas-medium testing machine equipped with a torsion actuator module.;Prior (D1) and subsequent (D2) deformation are accomplished by two torsion experiments in sequence on same sample segments. The effect of D1 strain history is investigated during D2 by applying counter-clockwise torsion to a sandwich sample consisting of three segments with different D1 rotation sense. D2 samples experienced continued, first and reversed shearing deformation in top, centre and bottom segments, respectively. D2 bulk strain was chosen equal to D1 strain in top and bottom segments.;D1 experiments followed the typical single-stage deformation behaviour of Carrara marble under the applied experimental conditions. Yielding was followed by strain hardening until a peak stress was reached at a shear strain around 1, after which work softening occurred. Weakening gradually evolved into a constant stress regime. During hardening, a shear microstructure and crystallographic preferred orientation (CPO) developed. Afterwards the volume fraction of smaller dynamic recrystallised grains increased continuously, resulting in a recrystallisation microstructure and CPO at shear strains of 5 and higher. The new D2 experiments displayed a strain variation between homogeneously deformed sample segments that increased with increasing D1 strain. The stress-strain behaviour of the D2 bulk sandwich samples showed less pronounced work-hardening and -softening when compared with single-stage deformation experiments. Furthermore, constant flow stress was attained at increasingly lower strain with increasing D1 strain. In most D2 segments, fabric development is equivalent to single-stage experiments at corresponding absolute strain. The fabrics differed markedly from those in single-stage experiments in the case of reversed two-stage deformation at moderate strain (D1 shear strain 1 and 2.6). Experiments show that grain shape by shearing of relict grains is defined by finite strain and thus affected by strain reversal. Recrystallisation is controlled by absolute strain and not influenced by strain reversal.
ISSN: 0040-1951

hal-00617686
https://hal.archives-ouvertes.fr/hal-00617686
DOI : 10.1016/j.tecto.2010.09.029

Résumé : The slides were taken on collecting trips sponsored by the William L. Bryant Foundation, where books, music and art indigenous to the regions were gathered. The are organized by geographical location.
This statue is located at el Palacio de los Capitanes Generales in Havana, Cuba. The palace used to house the captain general, or governor of Cuba when the island was under Spanish control. It is located on calle tacon near obispo, in old Havana.
Christopher Columbus marble monument was installed in the year 1862 by the Italian sculptor J. Cucchiari.
Cuba -- Caribbean region -- Havana

Droits : All rights to images are held by the respective holding institution. This image is posted publicly for non-profit educational uses, excluding printed publication. For permission to reproduce images and/or for copyright information contact Special Collections & University Archives, University of Central Florida Libraries, Orlando, FL 32816 phone (407) 823-2576, email: speccoll@mail.ucf.edu
CFM1972_01a
Sheet 85: 8
http://ufdc.ufl.edu/CA01200474/00001

Résumé : (Ownership) Received by the Rubenstein Library as a gift from Holly Ackerman in 2009. Photographed by Sergio Lastres.
In December 1994, a public monument, called the Liberty Column, was inaugurated in Miami commemorating the journey and suffering of Cuban rafters. Designed by sculptor Enzo Gallo, the statue consists of hands raised to the sky and a round marble column set in a fountain. It is located at Bay Front Park in Miami in front of the Hotel Intercontinental. The statue was vandalized in 2004 and restored by Cuban-American sculptor Marc Andries Smit. The plaque beside the monument reads, “Since 1959, thousands of Cubans have perished anonymously while fleeing tyranny in small boats and makeshift rafts although their names, like martyred refugees of other nations, are written solely on the pages of the sea, this column is a permanent testimony of the human need to be free.”

Éditeur(s) : Paris : Marpon et Flammarion Paris : Marpon et Flammarion
Résumé : At head of title: Un peuple noir devant les peuples blancs (étude de politique et de sociologie comparées)
This item is part of the West Indies collection.
Half leather with marbled boards and endpapers; raised bands and gold stamping on spine; inscription by author on preliminary page.

Droits : All rights to images are held by the respective holding institution. This image is posted publicly for non-profit educational uses, excluding printed publication. For permission to reproduce images and/or for copyright information contact Special Collections & University Archives, University of Central Florida Libraries, Orlando, FL 32816 phone (407) 823-2576, email: speccoll@mail.ucf.edu
UCF Special Collections Bryant - 5th Floor -- F1921.J36 1883
DP0003448

Résumé : (Ownership) Received by the Rubenstein Library as a gift from Holly Ackerman in 2009. Photographed by Sergio Lastres.
In December 1994, a public monument, called the Liberty Column, was inaugurated in Miami commemorating the journey and suffering of Cuban rafters. Designed by sculptor Enzo Gallo, the statue consists of hands raised to the sky and a round marble column set in a fountain. It is located at Bay Front Park in Miami in front of the Hotel Intercontinental. The statue was vandalized in 2004 and restored by Cuban-American sculptor Marc Andries Smit. The plaque beside the monument reads, “Since 1959, thousands of Cubans have perished anonymously while fleeing tyranny in small boats and makeshift rafts although their names, like martyred refugees of other nations, are written solely on the pages of the sea, this column is a permanent testimony of the human need to be free.”
Cuba

Résumé : Written on verso: "Statue of Havana fountain, an Indian maiden, Colon Park."
1910-1930
CHC5017
Havana (Cuba)

Droits : http://merrick.library.miami.edu/digitalprojects/copyright.html
chc50170002820001001
1290

Éditeur(s) : HAL CCSD Springer
Résumé : International audience
Thermoelastic behavior of different marble types was analyzed using computational modeling and experimental measurements. Eight marble samples with different composition, grain size, grain boundary geometry, and texture were investigated. Calcitic and dolomitic marbles were considered. The average grain size varies from 75 μm to 1.75 mm; grain boundary geometry differs from nearly equigranular straight grain boundaries to inequigranular-interlobate grain boundaries. Four typical marble texture types were observed by EBSD measurements: weak texture; strong texture; girdle texture and high-temperature texture. These crystallographic orientations were used in conjunction with microstructure-based finite element analysis to compute the thermoelastic responses of marble upon heating. Microstructural response maps highlight regions and conditions in the marble fabric that are susceptible to degradation phenomena. This behavior was compared to the measured thermal expansion behavior, which shows increasing residual strains upon repetitive heating-cooling cycles. The thermal expansion behavior as a function of temperature changes can be classified into four categories: (a) isotropic thermal expansion with small or no residual strain; (b) anisotropic thermal expansion with small or no residual strain; (c) isotropic thermal expansion with a residual strain; and (d) anisotropic thermal expansion with residual strain. Thermal expansion coefficients were calculated for both simulated and experimental data and also modeled from the texture using the MTEX software. Fabric parameters control the amount and directional dependence of the thermal expansion. Marbles with strong texture show higher directional dependence of the thermal expansion coefficients and have smaller microstructural values of the maximum principal stress and strain energy density, the main precursors of microcracking throughout the marble fabric. In contrast, marbles with weak texture show isotropic thermal expansion behavior, have a higher propensity to microcracking, and exhibit higher values of maximum principal stress and strain energy density. Good agreement between the experimental and computational results is observed, demonstrating that microstructure-based finite-element simulations are an excellent tool for elucidating influences of rock fabric on thermoelastic behavior.
ISSN: 1866-6280

hal-00858095
https://hal.archives-ouvertes.fr/hal-00858095
DOI : 10.1007/s12665-013-2406-z

Résumé : The slides were taken on collecting trips sponsored by the William L. Bryant Foundation, where books, music and art indigenous to the regions were gathered. The are organized by geographical location.
The Rodney Memorial, flanked by two canons, was built to commemorate the victory of Admiral Lord George Brydges Rodney in the Battle of the Saints in 1782. The marble statue was designed by the English sculptor John Bacon and features Rodney wearing a Roman tunic and stands in Spanish Town, Saint Catherine, Jamaica. Slide labeled Spanish Town.
Jamaica -- Caribbean region -- Spanish Town, Saint Catherine

Droits : All rights to images are held by the respective holding institution. This image is posted publicly for non-profit educational uses, excluding printed publication. For permission to reproduce images and/or for copyright information contact Special Collections & University Archives, University of Central Florida Libraries, Orlando, FL 32816 phone (407) 823-2576, email: speccoll@mail.ucf.edu
CFM1972_01a
http://ufdc.ufl.edu/AA00031102/00001

Résumé : The slides were taken on collecting trips sponsored by the William L. Bryant Foundation, where books, music and art indigenous to the regions were gathered. The are organized by geographical location.
This photograph shows a large building which is part of Havana's public square, which was originally called la Plaza Cívica (Civic Square), but after the Cuban Revolution was renamed "Plaza de la Revolución" or "Revolution Square." The large tower is a memorial to Jose Marti, which was erected during the Presidency of Fulgencio Batista. The square and the memorial were completed in 1959, the year that Fidel Castro came to power. This picture includes many vehicles of the 1950. In front of the building are two billboards. The billboard on the right is a political ad for, then president Batista. It reads "Paz, Trabajo, progreso" - meaning "Peace, Work and Progress."
The 109 m (358 ft) tower, designed by a team of architects led by Enrique Luis Varela, is in the form of a five-pointed star, encased in grey Cuban marble from the Isla de la Juventud.
Cuba -- Caribbean region -- Havana

Droits : All rights to images are held by the respective holding institution. This image is posted publicly for non-profit educational uses, excluding printed publication. For permission to reproduce images and/or for copyright information contact Special Collections & University Archives, University of Central Florida Libraries, Orlando, FL 32816 phone (407) 823-2576, email: speccoll@mail.ucf.edu
CFM1972_01a
Sheet 26: 17
http://ufdc.ufl.edu/CA01200416/00001

Éditeur(s) : Printed at the Chiswick Press by C. Whittingham, for J. Carpenter, Old Bond Street J. Booker, New Bond Street Sharpe and Hailes, Museum, Piccadilly and Gale, Curtis, and Fenner, Paternoster Row Printed at the Chiswick Press by C. Whittingham, for J. Carpenter, Old Bond Street J. Booker, New Bond Street Sharpe and Hailes, Museum, Piccadilly and Gale, Curtis, and Fenner, Paternoster Row ( [London] )
Résumé : (Citation/Reference) NUC pre-1956
(Statement of Responsibility) written by himself.
Spine title: Robinson Crusoe.
Variant of Lovett, R.W. Robinson Crusoe, 192 which has v.1: [2] unnumbered pages, p. iii-xvi, life of Defoe; v.2: p. 1-369. Library's copy v.1: [4] unnumbered pages, p. [v]-xvi, Life of Daniel Defoe; v.2: lacking half-title p., p. 1-360.
In marbled contemporary boards, three-quarter morocco, gilt relief decorative spines, marbled endpapers.
Parts I and II of Robinson Crusoe. Part II originally published under title: Farther adventures of Robinson Crusoe.
(Funding) NEH RLG GCMP4
England -- London

Droits : This item is presumed to be in the public domain. The University of Florida George A. Smathers Libraries respect the intellectual property rights of others and do not claim any copyright interest in this item. Users of this work have responsibility for determining copyright status prior to reusing, publishing or reproducing this item for purposes other than what is allowed by fair use or other copyright exemptions. Any reuse of this item in excess of fair use or other copyright exemptions may require permission of the copyright holder. The Smathers Libraries would like to learn more about this item and invite individuals or organizations to contact The Department of Special and Area Studies Collections (special@uflib.ufl.edu) with any additional information they can provide.
001801284
29632392
AJM5045

Éditeur(s) : HAL CCSD Elsevier Masson
Résumé : International audience
Although they are famous among Earth scientists, the Lherz peridotites are exposed within geological formations of the North Pyrenean Zone (NPZ) still lacking detailed investigations. Our study focuses on the metasediments of the Aulus basin hosting the Lherz peridotite body and associated ultramafic fragments of smaller size. The new data set comprises of structural analysis and detailed geological mapping of the massive Mesozoic marbles that form the prerift sequence typical of the NPZ and of the ultramafic-rich clastic breccia formations surrounding the peridotite bodies. The massive marbles display an evolution from hot and ductile to cold and brittle deformation, indicative of an exhumation process ending with the sedimentary reworking of both the deformed Mesozoic metasediments and the exhumed ultramafic rocks. Crystal Preferred Orientations (CPO) measured in the marbles support a deformation mechanism by dislocation creep of calcite, which is dominant between 400 8C and 600 8C; these deformation temperatures are within the range determined earlier by Clerc et al. (2015), using RSCM (Raman Spectroscopy of Carbonaceous Material) geothermometry. As a consequence, we better describe the transition from ductile to brittle deformation in the prerift marbles and clarify the origin of the syn-rift breccias. Due to continuous exhumation along detachments' faults, the brecciated metamorphic carbonates of the prerift NPZ sedimentary cover were passively uplifted towards shallower levels and progressively unroofed, while transported passively on the back of the exhumed ultramafic footwall. These results are consistent with the recent interpretations of the North Pyrenean peridotites as remnants of subcontinental mantle rocks exhumed within the pre-Pyrenean rift system. We emphasize the importance of tectonic decoupling between the Mesozoic sedimentary cover and the Palaeozoic basement, which leads to the juxtaposition of metamorphosed and deformed Mesozoic Please cite this article in press as: Lagabrielle Y, et al. Very high geothermal gradient during mantle exhumation recorded in mylonitic marbles and carbonate breccias from a Mesozoic Pyrenean palaeomargin (Lherz area, North Pyrenean Zone, France). C. R. Geoscience (2016), http://dx.
ISSN: 1631-0713

Droits : http://creativecommons.org/licenses/by-nc-nd/
insu-01285079
https://hal-insu.archives-ouvertes.fr/insu-01285079
https://hal-insu.archives-ouvertes.fr/insu-01285079/document
https://hal-insu.archives-ouvertes.fr/insu-01285079/file/1-s2.0-S1631071315002060-main.pdf
DOI : 10.1016/j.crte.2015.11.004

Éditeur(s) : HAL CCSD Société géologique de France
Résumé : In the eastern Pyrenees, the lherzolites always outcrop as restricted bodies scattered across Mesozoic sedimentary units along the North Pyrenean fault. In this article, we focus on the sedimentary processes associated with the tectonic exhumation of the mantle rocks during the Lower Cretaceous and we provide a new detailed analysis of the ultramafic-bearing sedimentary sequences associated with the Lherz body. The Lherz body, 1.5 km long only, belongs to a series of ultramafic bodies of restricted size (a few m to some hundred of m), occurring within sedimentary formations composed mostly of carbonate breccias originating from the reworking of Mesozoic platform limestones and dolomites. The carbonate clasts include marbles displaying different evolutions in relation with the Cretaceous thermal metamorphic event. The clastic formations also include numerous layers of polymictic breccias reworking ultramafic clasts. These layers are found far from any peridotitic body, implying that ultramafic clasts have been transported far away from their sources by sedimentary processes after their disaggregation on the seafloor. In addition, clasts of ultramafic-rich breccias and sandstones are also observed which indicates rapid sedimentation and diagenesis within a tectonically active environment. We discuss the significance of these deposits and their bearing on our understanding of the tectono-sedimentary processes associated with mantle exhumation in a context of development of narrow intracontinental basins suffering extreme crustal thinning.
EISSN: 1777-5817

hal-00766884
https://hal.archives-ouvertes.fr/hal-00766884
DOI : 10.2113/gssgfbull.183.5.443

Éditeur(s) : Printed for J.F. Dove Printed for J.F. Dove ( London (Piccadilly opposite Burlington House) )
Résumé : (Statement of Responsibility) with twenty-two engravings & a life of the author /|by the Revd. H. Stebbing.
Spine title: Robinson Crusoe : 22 plates; running title: Robinson Crusoe, complete edition; caption title, p. 263: Farther adventures of Robinson Crusoe.
Appears to be an earlier edition of Lovett, R.W. Robinson Crusoe, 329. Based upon similarity, plates probably designed by H. Corbould and engraved by C. Rolls.
Parts I and II of Robinson Crusoe. Part II originally published under title: Farther adventures of Robinson Crusoe.
Cloth boards with morocco spine; marbled edges.
Library's copy imperfect: wanting frontispiece.
England -- London

Droits : This item is presumed to be in the public domain. The University of Florida George A. Smathers Libraries respect the intellectual property rights of others and do not claim any copyright interest in this item. Users of this work have responsibility for determining copyright status prior to reusing, publishing or reproducing this item for purposes other than what is allowed by fair use or other copyright exemptions. Any reuse of this item in excess of fair use or other copyright exemptions may require permission of the copyright holder. The Smathers Libraries would like to learn more about this item and invite individuals or organizations to contact The Department of Special and Area Studies Collections (special@uflib.ufl.edu) with any additional information they can provide.
12646068

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Tethyan ophiolites show an apparent poorly organized association of ultramafic andmafic rocks. By contrast tothe complete mantle-crustal sections of Semail-type ophiolite sheets, Tethyan ophiolites are characterized by asmaller amount of mafic rocks (gabbros and basalts), by the absence of any sheeted dyke complex and by thefrequent occurrence of oceanic sediments stratigraphically overlying mantle-derived peridotites and associatedgabbroic intrusions. Therefore, they are considered as typical remnants of oceanic lithosphere formed in slowspreadingenvironment or in ocean–continent transition at distal passive margins. In the very first models offormation of the Tethyan ophiolites, in the years 1980, the geodynamical processes leading to mantle unroofingwere poorly understood due to the paucity of data and concepts available at that time from the present-dayoceans. In particular, at that time, little work had focused on the distribution, origin and significance ofmafic rocks with respect to the dominant surrounding ultramafics. Here, we reconsider the geology of sometypical metaophiolites from the Western Alps and Corsica, and we show how results from the past decadeobtained in the current oceans ask for reassessing the significance of the Tethyan ophiolites in general. Revisitedexamples include a set of representative metaophiolites from the blueschists units of the Western Alps (Queyrasregion) and from Alpine Corsica (Golo Valley). Field relationships between the ophiolitic basement andthe metasedimentary/metavolcanic oceanic cover are described, outlining a typical character of the Tethyanophiolite lithological associations. Jurassic marbles and polymictic ophiolite metabreccias are unconformablyoverlying the mantle-gabbo basement, in a way strictly similar to what is observed in the non-metamorphicAppennine ophiolites or Chenaillet massif. This confirms that very early tectonic juxtaposition of ultramafic andmafic rocks occurred in the oceanic domain before subduction. This juxtaposition resulted from tectonic activitythat is now assigned to the development of detachment faults and to the formation of Oceanic Core Complexes(OCCs) at the axis of slow spreading ridges. This fundamental Plate Tectonics process is responsible for the exhumationand for the axial denudation of mantle rocks and gabbros at diverging plate boundaries. In addition, fieldrelationships between the discontinuous basaltic formations and the ultramafic–mafic basement indicate that thistectonic stage is followed or not by a volcanic stage.We discuss this issue in the light of available field constraints.
ISSN: 0012-8252

insu-01096467
https://hal-insu.archives-ouvertes.fr/insu-01096467
https://hal-insu.archives-ouvertes.fr/insu-01096467/document
https://hal-insu.archives-ouvertes.fr/insu-01096467/file/Lagabrielle-EarthSciRev-2014.pdf
DOI : 10.1016/j.earscirev.2014.11.004

Éditeur(s) : HAL CCSD Geological Society of America
Résumé : International audience
Fluid-rock interactions can control earthquake nucleation and the evolution of earthquake sequences. Experimental studies of fault frictional properties in the presence of fluid can provide unique insights into these interactions. We report the first results from experiments performed on cohesive silicate-bearing rocks (microgabbro) in the presence of pressurized pore fluids (H2O, drained conditions) at realistic seismic deformation conditions. The experimental data are compared with those recently obtained from carbonate-bearing rocks (Carrara marble). Contrary to theoretical arguments, and consistent with the interpretation of some field observations, we show that frictional melting of a microgabbro develops in the presence of water. In microgabbro, the initial weakening mechanism (flash melting of the asperities) is delayed in the presence of water; conversely, in calcite marble the weakening mechanism (brittle failure of the asperities) is favored. This opposite behavior highlights the importance of host-rock composition in controlling dynamic (frictional) weakening in the presence of water: cohesive carbonate-bearing rocks are more prone to slip in the presence of water, whereas the presence of water might delay or inhibit the rupture nucleation and propagation in cohesive silicate-bearing rocks.
ISSN: 0091-7613

hal-01054327
https://hal.archives-ouvertes.fr/hal-01054327
DOI : 10.1130/G34916.1

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Slices of polycyclic metasediments (marbles and meta-cherts) are tectonically amalgamated with the polydeformed basement of the Dent Blanche tectonic system along a major Alpine shear zone in the Western Alps (Becca di Salé area, Valtournenche Valley). A combination of techniques (structural analysis at various scales, metamorphic petrology, geochronology and trace element geochemistry) was applied to determine the age and composition of accessory phases (titanite, allanite and zircon) and their relation to major minerals. The results are used to reconstruct the polyphase structural and metamorphic histories, comprising both pre-Alpine and Alpine cycles. The pre-Alpine evolution is associated with low-pressure high-temperature metamorphism related to Permo-Triassic lithospheric thinning. In meta-cherts, microtextural relations indicate coeval growth of allanite and garnet during this stage, at ~ 300 Ma. Textures of zircon also indicate crystallisation at HT conditions; ages scatter from 263 to 294 Ma, with a major cluster of data at ~ 276 Ma. In impure marble, U-Pb analyses of titanite domains (with variable Al and F contents) yield apparent 206Pb/238U dates range from Permian to Jurassic. Chemical and isotopic data suggest that titanite formed at Permian times and was then affected by (extension-related?) fluid circulation during the Triassic and Jurassic, which redistributed major elements (Al and F) and partially opened the U-Pb system. The Alpine cycle lead to early blueschist facies assemblages, which were partly overprinted under greenschist facies conditions. The strong Alpine compressional overprint disrupted the pre-Alpine structural imprint and/or reactivated earlier structures. The pre-Alpine metamorphic record, preserved in these slices of metasediments, reflects the onset of the Permo-Triassic lithospheric extension to Jurassic rifting.
ISSN: 0024-4937

hal-00758123
https://hal.archives-ouvertes.fr/hal-00758123
DOI : 10.1016/j.lithos.2012.05.007

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
ISSN: 0169-1368

hal-00329701
https://hal.archives-ouvertes.fr/hal-00329701
DOI : 10.1016/j.oregeorev.2008.03.003