Éditeur(s) : J. Humphreys J. Humphreys ( Philadelphia )
Résumé : Accompanied by "A new atlas of the British West Indies, with a whole sheet general map of the West India Islands, and a whole sheet map of the Island of Hispaniola or St. Domingo, engraved to accompany the Philadelphia edition of Edwards History of the West Indies." (2 p.l., 11 maps (part fold.) 29 x 28 cm)
4 v. front. (port.) tables (part fold.) 21 cm.

Droits : Per item in Hathi Trust, item is in the public domain: http://catalog.hathitrust.org/Record/002241056
1915482
http://ufdc.ufl.edu/AA00019357/00004

Éditeur(s) : HAL CCSD Elsevier
Résumé : Folds with hinge lines subparallel to stretching lineation are common features in shear zones and represent extreme cases of fold modification. However, their microstructures and in particular their kinematic significance remain poorly understood. Here we describe the meso- and micro-scale structures and crystallographic preferred orientation (CPO) of quartz and muscovite from a metric-scale shear-modified fold from Plattjen, Saas Fee, Western Internal Alps. The studied fold is of class-2 and the samples collected around the fold have essentially the same microstructures. Quartz [c]-axes plotted in the tectonic coordinate system exhibit an apparent reverse obliquity on opposing limbs. Muscovite fabrics are controlled essentially by the orientation of {001} planes. If the CPO data are plotted in a common reference frame (e.g. either fold or geographical), all samples exhibit essentially the same patterns for both minerals. In particular, relative to the fold axis and axial surface, the reversal of quartz CPO obliquity on opposing limbs is no longer evident. The small obliquity (~ 15°) between the intersection lineation of the two planes of {001} of muscovite and the fold axis results in the apparent reversal of shear sense on opposite limbs when viewing the CPO related to the macroscopic fabric. The homogeneity of the microstructures and CPOs of quartz and muscovite across the fold support the interpretation that the fold developed during simultaneous activation of heterogeneous and homogeneous simple shear, with the former responsible for fold development and the latter responsible for fold rotation and the overwhelming of the heterogeneous deformation. These processes led to the observed parallelism between fold hinge line and local stretching lineation.
ISSN: 0040-1951

hal-00824537
https://hal.archives-ouvertes.fr/hal-00824537
DOI : 10.1016/j.tecto.2011.03.003

Résumé : The Tobacco sorter sorts tobacco leaves according to color and condition for use as cigar wrappers or binders: Selects leaves without obvious defects from bundle and lays them on booker bench (curved-top stand over which leaves are draped). Examines leaves for color variations, tears, tar spots, tight grain, and size under specifications. Places leaves not suitable for wrapper in separate pile. Folds wrapper leaves into bundles for stripping.
(Funding) Funded in part by the Institute for Museum and Library Services (IMLS), Ephemeral Cities Project.
Tampa |z 1271000 |2 ceeus
Hillsborough County |z 12057 |2 ceeus
United States of America -- Florida -- Hillsborough County -- Tampa

Droits : All rights reserved. 2005.
C24-05745

Éditeur(s) : J. Humphreys J. Humphreys ( Philadelphia )
Résumé : Accompanied by "A new atlas of the British West Indies, with a whole sheet general map of the West India Islands, and a whole sheet map of the Island of Hispaniola or St. Domingo, engraved to accompany the Philadelphia edition of Edwards History of the West Indies." (2 p.l., 11 maps (part fold.) 29 x 28 cm)
4 v. front. (port.) tables (part fold.) 21 cm.

Droits : Per item in Hathi Trust, item is in the public domain: http://catalog.hathitrust.org/Record/002241056
1915482
http://ufdc.ufl.edu/AA00019357/00001

Éditeur(s) : El Ministerio El Ministerio ( Caracas )
Résumé : (Additional Physical Form) Also issued on microfilm from Library of Congress Preservation Microfilming Program.
(Numbering Peculiarities) Report year ends in April.
(Numbering Peculiarities) No report published in 1906.
(Issuing Body) 18??-18?? issued by Ministerio de lo Interior y Justicia; 18??- by Ministerio de Relaciones Interiores.
Part of illustrative material is folded.
The dates given are those on the title-pages, corresponding to the date of transmittal of reports, which are usually for the preceding fiscal years.
Venezuela
Venezuela
Venezuela
Venezuela

01643059
45040626
ocm01643059
http://ufdc.ufl.edu/AA00016875/00001

Éditeur(s) : HAL CCSD American Geophysical Union
Résumé : International audience
Large-scale periodic undulations within the oceanic and continental lithospheres revealed by a number of observations, are often treated as compressive instabilities, i.e. lithospheric buckling or folding. These undulations are normally associated with intensive faulting, which raises questions on the role of faulting in the folding process, and even on the possibility of folding in highly faulted media. In this study, we demonstrate that folding can "survive" faulting and that both processes may develop concurrently, so that faulting may serve as a mechanism of folding in the brittle domain. We support this hypothesis by direct numerical modeling. The results are compared with the data on three most prominent and well-known cases of the oceanic and continental folding-like deformation ("Indian Ocean" type, "Western Gobi (central Asia)" type and "Central Australian" type). We demonstrate that under reasonable tectonic stresses, folds can develop from faults cutting through the brittle parts of the lithosphere. The predicted wavelengths and nite growth rates are in agreement with the observations. We also show that within a continental lithosphere with thermotectonic age greater than 400 My, either a bi-harmonic mode (two superimposed wavelengths, crustal and mantle one) or a coupled mode (mono-layer deformation) of inelastic folding can develop, depending on the strength and thickness of the lower crust.
ISSN: 0094-8276

ird-00388016
http://hal.ird.fr/ird-00388016
http://hal.ird.fr/ird-00388016/document
http://hal.ird.fr/ird-00388016/file/fig3.pdf
http://hal.ird.fr/ird-00388016/file/fig1.pdf

Résumé : Library copy included with three other maps folded to 27 x 19 cm. in box with title: Isle Saint Domingue.
Library copy dissected and mounted on cloth.
Hand-coloring distinguishes masonry, wood and projected structures.
"Le Cap à l'eglise méridienne 74d 38m 25s, latitude 19d 46m 24s" ; revised from Paris to Greenwich meridian in this description.
"Dédié à Monseigneur Le Maréchal de Castries, chevalier des ordres du Roi, ministre et secrétaire d'etat de la marine, par son très humble et très respectueux serviteur René Phelipeau, géographe, rue de la Harpe près celle du foin."
Includes inset drawing of bridge spanning the Haut du Cap river.
Oriented with North to the right.
Relief shown by hachures and shading. Depths shown by soundings.

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 Digital Services (UFDC@uflib.ufl.edu) with any additional information they can provide.
77008219
http://ufdc.ufl.edu/UF00028442/00001

Éditeur(s) : HAL CCSD Geological Society of London
Résumé : The Zagros Simply Folded Belt (ZSFB) is an active fold-and-thrust belt resulting from the still continuing continental collision between the Arabian plate and the Iranian plate, which probably started in the Oligocene. The present-day shortening (N25°) is well documented by focal mechanisms of earthquakes and global positioning system (GPS) surveys. We propose in this study a comparison of published palaeostress markers, including magnetic fabric, brittle deformation and calcite twinning data. In addition, we describe the magnetic fabric from Palaeocene carbonates (10 sites) and Mio-Pliocene clastic deposits (15 sites). The magnetic fabrics are intermediate, with magnetic foliation parallel to the bedding, and a magnetic lineation mostly at right angles to the shortening direction. This suggests that the magnetic fabric retains the record of an early layer-parallel shortening (LPS) that occurred prior to folding. The record of LPS allows the identification of originally oblique folds such as the Mand Fold, which have developed in front of the Kazerun Fault. The shape parameter of the magnetic fabric indicates a weak strain compatible with the development of detachment folds in the ZSFB. The palaeostress datasets, covering the Palaeocene to Pleistocene time interval, support several folding episodes accompanied by a counter-clockwise rotation of the stress field direction. The Palaeocene carbonates in the ZSFB record a N47 LPS during early to middle Miocene detachment folding in the High Zagros Belt (HZB). The Mio-Pliocene clastic deposits recorded a N38 LPS prior to and during detachment folding within the ZSFB at the end of the Miocene-Pliocene. Similarly, fault slip and calcite twin data from the ZSFB also support a counter-clockwise rotation from NE to N20 between the pre-folding stage and the late rejuvenation of folds. This counter-clockwise trend of palaeostress data agrees with fault slip data from the HZB. During the late stage of folding in the ZSFB, the Plio-Quaternary palaeostress trends are consistently parallel to the present-day shortening direction.
Tectonic and stratigraphic evolution of Zagros and Makran during the Mesozoic-Cenozoic

hal-00545036
https://hal.archives-ouvertes.fr/hal-00545036
DOI : 10.1144/SP330.6

Éditeur(s) : [s.n.] [s.n.] ( México )
Résumé : "Tira de la Peregrinación azteca": fold. strip in pocket of v. 3.
Mexico
Mexico
Mexico

03171808
48023620

Éditeur(s) : El Ministerio El Ministerio ( Caracas )
Résumé : (Additional Physical Form) Also issued on microfilm from Library of Congress Preservation Microfilming Program.
(Numbering Peculiarities) Report year ends in April.
(Numbering Peculiarities) No report published in 1906.
(Issuing Body) 18??-18?? issued by Ministerio de lo Interior y Justicia; 18??- by Ministerio de Relaciones Interiores.
Part of illustrative material is folded.
The dates given are those on the title-pages, corresponding to the date of transmittal of reports, which are usually for the preceding fiscal years.
Venezuela
Venezuela
Venezuela
Venezuela

01643059
45040626
ocm01643059
http://ufdc.ufl.edu/AA00016875/00001

Éditeur(s) : El Ministerio El Ministerio ( Caracas )
Résumé : (Additional Physical Form) Also issued on microfilm from Library of Congress Preservation Microfilming Program.
(Numbering Peculiarities) Report year ends in April.
(Numbering Peculiarities) No report published in 1906.
(Issuing Body) 18??-18?? issued by Ministerio de lo Interior y Justicia; 18??- by Ministerio de Relaciones Interiores.
Part of illustrative material is folded.
The dates given are those on the title-pages, corresponding to the date of transmittal of reports, which are usually for the preceding fiscal years.
Venezuela
Venezuela
Venezuela
Venezuela

01643059
45040626
ocm01643059
http://ufdc.ufl.edu/AA00016875/00001

Éditeur(s) : Printed for the Hakluyt society Printed for the Hakluyt society ( London )
Résumé : (Statement of Responsibility) by Father Joseph de Acosta. Reprinted from the English translated edition of Edward Grimestone, 1604. And ed., with notes and an introduction, by Clements R. Markham.
Paged continuously.
The folded map, issued with v. 1, has half-title: ... Map of Peru; to illustrate the Travels of Cieza de Leon, in 1532-50; The royal commentaries of Garcilasso de la Vega (1690); and the Natural and moral history of the Indies, by Father Joseph de Acosta (1608) [nos. 33, 41, 45, 60, and 61 of the society's publications] Included t.-p. translated from Madrid edition, 1608; followed by t.-p. of London edition, 1604.
Peru
Spanish America
America
Latin America

001642703
01616105
AHV4172
05040450

Éditeur(s) : Gauthier-Villars
Résumé : The variability of ''yellow substance'' in waters of the Skagerrak and the Kattegat was studied during the international Skagex programme in 1990 and 1991. Data on attenuation of light and fluorescence of dissolved organic matter (DOM) in sea water were collected with a spectral transmissiometer and a submersible fluorometer within a depth range of 0-250 m at several stations. More than fifty-fold variations of fluorescence intensity over space and time were due to the combined action of different sources of DOM in the straits. The surface maximum of fluorescing DOM, related to river outflow, was spreading from Oslo fjord to the central Skagerrak in late spring. This maximum may be ecologically important because it diminishes shortwave PAR. In the autumn the brightest DOM fluorescence was found in the Kattegat and along the Norwegian coast in accordance with earlier studies. The local minima of DOM fluorescence are associated with the Jutland current. Both the instability of the current and a ten-fold difference in DOM content between deep layers of the Skagerrak and Kattegat resulted in strong synoptic variability of fluorescence in the transitional area between the straits. Seasonal and synoptic variabilities of ''yellow substance'' were minimal in the southern Kattegat. The vertical gradients of DOM fluorescence were mostly negative at the depth of the thermocline of the open Skagerrak in spring, reaching values of 40-50 % m-1. Fine structure and complex shape were inherent to fluorescence profiles from areas of intensive water mixing. DOM fluorescence closely covaried with attenuation of UV light: the correlation coefficient was + 0.9 for wavelength w <= 350 nm regardless of season. The inverse dependence between wavelength derivative and magnitude of UV attenuation in the straits did not change with season. DOM fluorescence and water salinity were negatively correlated at depths of 25-50 m but they varied independently in the upper 10 m. No significant correlation between fluorescence and nitrates has been found. Estimates of correlation with phosphates ranged from 0.7 to 0.8. In general, the changes of fluorescence were due to variations of DOM content in sea water but not to variability of DOM composition or state. The properties of DOM fluorescence in the Skagerrak-Kattegat area make it a useful natural tracer of water movements suitable for active remote sensing with airborne lidar.
Oceanologica Acta (0399-1784) (Gauthier-Villars), 1993 , Vol. 16 , N. 2 , P. 115-125

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/00099/21041/18667.pdf
http://archimer.ifremer.fr/doc/00099/21041/

Éditeur(s) : N. V. Algemeene Boekhandel voor Inwendige en Uitwendige Zending N. V. Algemeene Boekhandel voor Inwendige en Uitwendige Zending ( 's-Gravenhage )
Résumé : (Statement of Responsibility) door H. G. Steinberg; met gedeeltelijke medewerking van G. J. Staal.
"De Suriname-zending; der Evangelische Broedergemeente in kaart; bijlage bei Ons Suriname" (24 p. of maps (1 fold.)) in pocket.
Includes indexes.
Suriname

000201644
AAW8400
03889494
25352503

Éditeur(s) : J. Humphreys J. Humphreys ( Philadelphia )
Résumé : Accompanied by "A new atlas of the British West Indies, with a whole sheet general map of the West India Islands, and a whole sheet map of the Island of Hispaniola or St. Domingo, engraved to accompany the Philadelphia edition of Edwards History of the West Indies." (2 p.l., 11 maps (part fold.) 29 x 28 cm)
4 v. front. (port.) tables (part fold.) 21 cm.

Droits : Per item in Hathi Trust, item is in the public domain: http://catalog.hathitrust.org/Record/002241056
1915482
http://ufdc.ufl.edu/AA00019357/00002

Éditeur(s) : HAL CCSD Elsevier
Résumé : We present comparative field studies in folded areas (Southern France. Moroccan Western Atlas and Abruzzo, Italy) giving new insights into fracture distribution within folded rocks of the shallow brittle crust. We show that the curvature in folds formed in brittle mechanical units is usually accommodated by multiple "dip-domain boundaries" (appearing as curvature discontinuities at fold scale) corresponding to relatively narrow and dense fracture zones, striking parallel or slightly oblique to the fold axis. They separate "dip-domains" where curvature is absent or moderate. It is shown that the dip-domain boundaries (which are obvious in the case of kink folds or box-fold anticlines) are currently present as multiple subtle hinges even when the curvature appears continuous at first sight. The nature of dip-domain boundaries is studied, they often cut through the whole thickness of the mechanical units Their internal structure varies, and a non-exhaustive typology is proposed For each type, an interpretative kinematic scenario shows how the dip-domain boundaries could initiate and develop. We suggest two kinds of origins (1) they could correspond to the reactivation of inherited, along-strike fracture zones (opening-mode fracture concentrations such as big joints, fracture corridors. Inherited faults, etc), (2) they could be created as mechanical instabilities during the fold formation (syn-folding origin), in particular through small reverse faults. In both cases, early zones of weakness localize the dip-domain boundaries, and control the Increase in curvature in association with increasing fracture density within the boundary. Because they represent well-defined vertically and axially persistent sub-seismic fracture zones generally limited to the thickness of the folded unit, dip-domain boundaries could enhance the axial permeability of folded and fractured reservoirs.
ISSN: 0191-8141

hal-00512651
https://hal.archives-ouvertes.fr/hal-00512651
DOI : 10.1016/j.jsg.2010.03.002

Éditeur(s) : El Ministerio El Ministerio ( Caracas )
Résumé : (Additional Physical Form) Also issued on microfilm from Library of Congress Preservation Microfilming Program.
(Numbering Peculiarities) Report year ends in April.
(Numbering Peculiarities) No report published in 1906.
(Issuing Body) 18??-18?? issued by Ministerio de lo Interior y Justicia; 18??- by Ministerio de Relaciones Interiores.
Part of illustrative material is folded.
The dates given are those on the title-pages, corresponding to the date of transmittal of reports, which are usually for the preceding fiscal years.
Venezuela
Venezuela
Venezuela
Venezuela

01643059
45040626
ocm01643059
http://ufdc.ufl.edu/AA00016875/00001

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The investigation of deformation rates on a mountain piedmont can provide key information for improving our understanding of the overall dynamics of a mountain range. Here, we estimate the shortening rate absorbed by a Quaternary emergent detachment fold on the southeastern piedmont of the Tianshan (China). Our work is primarily based on new 10Be cosmogenic exposure dating of deformed alluvial surfaces. The method we have developed combines depth profiling with sampling of surface cobbles, thereby allowing exposure time, erosion rate and inheritance to be simultaneously constrained. The exposure ages of the uppermost uplifted alluvial surfaces are around 140±17 ka140±17 ka, 130±9 ka130±9 ka and 47±9 ka47±9 ka, from west to east. A terrace lying below the 140 ka surface is dated at 65±5 ka65±5 ka. The ages of the uplifted and folded alluvial surfaces were then combined with estimates of shortening obtained using two distinct methods: (1) the excess area method, where sedimentation rates, extracted from magnetostratigraphic studies, are used to determine the amount of sedimentation after the abandonment of the river; and (2) a folding model derived from sandbox experiments. The late Pleistocene shortening rates are shown to be between 0.4±0.1 mm/yr0.4±0.1 mm/yr and 0.8±0.5 mm/yr0.8±0.5 mm/yr on the western part of the fold and 2.1±0.4 mm/yr2.1±0.4 mm/yr along its central part. The central part of the frontal Yakeng anticline therefore accommodates up to 25% of the total shortening currently absorbed across the whole Eastern Tianshan range (8 mm/yr). However, this situation seems to have prevailed for only the last 150 ka, as the shortening rate absorbed by this nascent fold was previously ten times slower. While the initiation of folding of the Yakeng anticline can be traced back to 5.5 Ma ago, the basinward migration of the active deformation front onto the Yakeng fold is a relatively recent phenomenon and appears to be diachronous from west to east, probably in relation to the tectonic activity of the folds in the hinterland.
ISSN: 0012-821X

hal-01306997
https://hal.archives-ouvertes.fr/hal-01306997
DOI : 10.1016/j.epsl.2015.11.041

Éditeur(s) : J. Humphreys J. Humphreys ( Philadelphia )
Résumé : Accompanied by "A new atlas of the British West Indies, with a whole sheet general map of the West India Islands, and a whole sheet map of the Island of Hispaniola or St. Domingo, engraved to accompany the Philadelphia edition of Edwards History of the West Indies." (2 p.l., 11 maps (part fold.) 29 x 28 cm)
4 v. front. (port.) tables (part fold.) 21 cm.

Droits : Per item in Hathi Trust, item is in the public domain: http://catalog.hathitrust.org/Record/002241056
1915482
http://ufdc.ufl.edu/AA00019357/00003

Éditeur(s) : El Ministerio El Ministerio ( Caracas )
Résumé : (Additional Physical Form) Also issued on microfilm from Library of Congress Preservation Microfilming Program.
(Numbering Peculiarities) Report year ends in April.
(Numbering Peculiarities) No report published in 1906.
(Issuing Body) 18??-18?? issued by Ministerio de lo Interior y Justicia; 18??- by Ministerio de Relaciones Interiores.
Part of illustrative material is folded.
The dates given are those on the title-pages, corresponding to the date of transmittal of reports, which are usually for the preceding fiscal years.
Venezuela
Venezuela
Venezuela
Venezuela

01643059
45040626
ocm01643059
http://ufdc.ufl.edu/AA00016875/00001