... author Dickinson once again proved his well-known humility and candidness by admitting that his own “initial supposition of timing of the sinistral slip Nacimiento fault zone had to stand revision, based on these findings” (p. 15). The engineering geologists on the author team are Lew Rosenberg...

...I. Kurzon; F. L. Vernon; A. Rosenberger; Y. Ben‐Zion Abstract We implement a new method for automatic detection of P and S phases using singular value decomposition ( SVD ) analysis. The method is based on the real‐time iteration algorithm of Rosenberger (2010) for the SVD of three‐component...

... 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...

... into west-central Vermont. Lower and middle Cambrian ages have been assigned to all units. The strata below the Gilman quartzite are tentatively correlated with the Mendon series in the Rutland-Brandon region. All units above the Gilman have stratigraphic equivalents in the adjoining Rosenberg succession...

... chevauchement de Rosenberg. Au Vermont, le chevauchement de Highgate Falls recoupe l’intérieur de l’anticlinal; ce chevauchement est irrégulier et présente un déplacement qui décroît en direction nord vers la frontière internationale. [Traduit par la Rédaction] The Champlain Thrust and related faults have...

... strike-slip faults, respectively. Simplon fault (SF) is another normal fault that caused orogen-parallel extension. (B) Map of central Brenner fault with location of surface samples (black circles) and sampled drill core (white square). Position of Brenner normal fault is after Rosenberg and Garcia...

...Figure 3. Depth structure map of top Edwards Formation with bubble chart of relative cumulative gas production for a selection of wells with 28 yr of production. The AA′ seismic line crosses the 1 Sobotik (S), 2 Sobotik (S2), and 6 Rosenberg (R) well (projected), with cumulative gas production...

...Claudio L. Rosenberg; Eduard Kissling Abstract Accommodation of collisional shortening in the Central Alps varies dramatically along strike, and this change is inferred to result from along-strike changes of rheology. In the western Central Alps, 90% of shortening is accommodated in the thickened...

... that emplaced high-grade, often partially molten GHS rocks southward over lower-grade LHS rocks. The STDS is a ductile to brittle fault system up to ~2 km thick, which juxtaposed low-grade THS rocks northward onto higher-grade GHS rocks ( F ig . 1 ). Thrust faults that internally deform the GHS package have...

...Erin E. Adlakha; Keiko Hattori Abstract The P2 fault, a 13 km-long steeply dipping reverse fault, is the main structural control of the McArthur River uranium deposit in the eastern Athabasca Basin, northern Saskatchewan, Canada. Three types of tourmaline were observed in the metasedimentary...

...Figure 4 Cross sections showing rift-parallel to rift-perpendicular orientations, and displaying variations in block rotation and fault dips, as would be expected for each orientation from this rift setting (e.g., Villamor and Berryman, 2001 ; Lamarche et al., 2006 ). Dikes using faults...