(2005) proposed that two radial (fanning) lineation patterns are seen in the Maiden Creek intrusion. (D) Zoom-in of (C) showing conjugate fractures in both intrusion and host rock. The shortening axis associated with these conjugate sets is however still consistent with the strain axis observed along the rest of the gully. Field photographs showing deformation structures at the intrusion-sandstone contact. The second type comprises large, tectonically driven structures (such as transtensional faults and/or shear zones) that form synchronously with magma emplacement, i.e., “syntectonic” accommodation structures (e.g., Hutton et al., 1990; McCaffrey, 1992; Neves et al., 1996; Passchier et al., 2005). In this model, the western and eastern lobes are offset lobate structures that form at the leading edge of two inclined, propagating sheets that most likely coalesce at depth (e.g., a saucer-shaped sill). If the MCSZ postdated emplacement of the intrusive bodies, we would expect to see a top-to-the-west offset of the altered sandstones relative to the underlying intrusive lobes. 6E–6I). (B) View from scan station 1, looking west. This results in the steepness of the central surface of the lens, an increase in thickness of the lens and a flattening of the lens edges. 6B and 9). Experts estimate that there are over 54,200 accommodation facilities in the United States alone. Area covered by models proposed in (B–D) shown. East–west–trending extensional structures observed in the southern part of Rattlesnake Gully are perpendicular to the dominantly constrictional deformation bands seen to the north (Fig. The age-related decline in accommodation occurs almost universally to less than 2 dioptres by the time a person reaches 45 to 50 years, by which time most of the population will have noticed a decrease in their ability to focus on close objects and hence require glasses for reading or bifocal lenses. Objects appear blurred in the plane behind the retina, but due to an increase in the optical power of the eyes, this object image becomes clear. In this model, magma propagates in a southerly direction from a main “sill-like” intrusive body situated to the NW. Geosphere ; 15 (4): 1368–1392. In essence, hospitality is made up of two services: the provision of overnight accommodation for people travelling away from home, and options for people dining outside their home. 2016); geochronological studies (e.g., Coleman et al., 2004; Westerman et al., 2004); magnetic and macroscopic fabric studies (e.g., de Saint Blanquat and Tikoff, 1997; Horsman et al., 2005; Stevenson et al., 2007); and integration of field and numerical modeling (e.g., Pollard and Johnson, 1973). It is bordered anteriorly (in front) by a ring it forms with the posterior side of the iris. (B) View looking north showing the Maiden Creek shear zone (MCSZ) sitting on the top surface of the two intrusive “lobes” and the Pussycat outcrop. 2, 4B, and 4C). Orientations roughly correspond to panoramic photograph views in (A) and (B). [16], In paralysis of accommodation, amplitude of accommodation is either markedly reduced or completely absent (cycloplegia). Fault planes were constructed in GoCAD™ (Fig. These fault planes trend parallel to the ∼N–S strike of the intrusion margin and dip shallowly (∼20°) to the west (Fig. 1). See our User Agreement and Privacy Policy. [15] Decreased accommodation may occur due to physiological (presbyopia), pharmacological (cycloplegia) or pathological. Therefore, changes in strain and deformation trends may reflect changes in the boundary conditions around the intrusion contacts: i.e., more contraction in the north where sandstones are trapped between two thick (>30 m) intrusive lobes and more extension in the south where the sandstones are less constrained due to the thinning (<10 m) and termination of the eastern lobe (Fig. 10). A far greater spread of measurements for bedding occurs in the gully below the MCSZ, where sandstones occur between the two intrusive lobes.
2).
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