..., respectively, in Vermont. In Quebec, the basal limestones have been inferred to be thrust over Cambrian dolomites (Gorge Formation in Vermont) of the Rosenberg slice, part of the parauthochthonous shelf, although this contact is not exposed there. In the Missisquoi River gorge of Vermont, a conformable...

... all formations are substantially redefined. The faunas of each formation are listed and reviewed. Structurally, the St. Albans area, which is basically a large northward-plunging syncline, is part of the Rosenberg thrust slice of Clark. East of the Champlain thrust six additional thrusts (four newly...

... convergence accommodation transitions from underplating and stacking of tectonic slices during slow subduction of the thin continental distal margin to widespread crustal shortening ( Rosenberg et al., 2018 ). The collision stage is inferred to be associated with the development of a foreland basin...

...). These rotations are represented at their site location on Figure 1 using a simple qualitative representation according to the nature of remanence. The uncertainty (dR) is indicated by a pie slice with an opening equal to two dR. Fig. 1 Synthetic structural map of the Western Alps. Major thrust and strike...

... (1995) described a very similar pattern along the South Armorican shear zone, but the exposed tails are strongly deformed in the solid state and may be tectonic slices along the fault. Additionally, Vigneresse (1995) argued that the true feeder systems can be imaged below the plutons as vertical...

... in the same genera ( Diaz and Rosenberg, 1995 ), but at about 0.5 ml/l most of the benthic macrofauna dies ( Rosenberg and others, 1991 ). Nilsson and Rosenberg (1998) refined that limit to 10% oxygen saturation. On the other hand several benthic foraminiferal species tolerate very low oxygen concentrations...

... and mechanical properties, but this can occur at quite low fluid fractions ( Rosenberg and Handy, 2005 ). Low P wave velocities in the upper mantle beneath the Anatolian Plateau and blockage of upper mantle S waves have also been attributed to partial melting ( Gök et al., 2003 ; Al-Lazki et al., 2004...

... of crystalline basement rocks. This is based on a number of thrust sheets selected from the different nappe systems, which are taken to be typical for the question addressed. The Helvetic nappe system comprises from top to bottom three major units: the Ultrahelvetic slices...

..., such as the overburden velocity, acquisition geometry, dip information, and reflectivity. It also identifies “geophysically invisible” interfaces that cannot be imaged despite improving the accuracy of migration algorithms or the velocity model. Rosenberg (2000) conducts a related study that analyzes the effects...

...Michael Garton; Duncan McIlroy Abstract This paper outlines a new method for the study of sedimentary fabrics in well-lithified facies. The technique involves the cutting of large, thin slices of rock that can then be viewed in transmitted light. The utility of this methodology is demonstrated...

... , 1977 ; LaBarbera, 1977 ; Stricker and Reed, 1985a , b ; Rosenberg et al., 1988 ; Alexander, 1990 ; Schumann, 1991 ; Daley, 1993 ) Both live and dead specimens were collected from each dredge that yielded brachiopods. For consistency, only whole, articulated shells of Terebratalia transversa...

... coordinates of a schor! (SCHI) de- termined by Fortier & Donnay (1975), an elbaite (ELB1) determined by Donnay & Barton (1972) and a dravite (DRVl ) determined by Foit & Rosenberg (1979) were selected for computer simulation. 2. Experimental methods Specimens for HRTEM study were prepared by grinding...

... are close to the ones at reservoir conditions. As a branch of petrophysics, digital rock technology developed rapidly. It can be used to describe the microstructure of reservoir rocks accurately ( Liu et al. 2009 ; Sun et al., 2012 ; Kong et al., 2015 ). Dunsmuir et al. (1991) , Rosenberg et al. (1999...

... episodes of anatexis: the first is phengite dehydration melting during the exhumation of deeply subducted slices, and the second is heating melting related to the post-orogenic collapse. Petrographic evidence and clues of the anatectic events include biotite + plagioclase + garnet ± amphibole intergrowth...

...). The virtual axial slices were reconstructed in 32-bit Tiff format, with an isotropic voxel size ranging from 21 to 30 µm (see Table 2 ) and using the commercial software DigiXCT (DIGISENS, France). Table 2. Voxel size for the different microtomographic data reconstructed for the mantle xenoliths...

... from site BY15 in the Gotland Deep (57.3200°N, 20.0500°E, 238 m water depth) on the same cruise. All cores were sliced under nitrogen at 0.5–2 cm resolution, and analyzed for C org by thermal combustion and for Mo, P, and Al by inductively coupled plasma–optical emission spectrometry (ICP-OES) after...

.... Figure 4. Time slices from three-dimensional seismic data cube showing average energy. Whitish shades indicate blanking of seismic reflection amplitudes. Blanking zone merges at depth with local high of accreted sediments represented by similar whitish shades of minimum average energy. Also see text...

... on the continental crust during burial and exhumation, the timing of partial melting initiation needs to be constrained, since the softening effect of partial melting is efficient for very low melt contents ( Rosenberg and Handy, 2005 ). Attempts to date partial melting via accessory mineral dating in leucosomes...