Oblique marginal

Description Herbaceous perennial with short rhizomes. Stems 60-100 cm tall, 4-sided, densely hairy below, scattered hairy above. Leaves opposite lower leaves petiolate, 13-15 cm long, 4-5 cm wide, obovate, bases oblique, margins crenate upper leaves sessile, ovate-lanceolate, 5-6 cm long, 2-3 cm wide, margins serrate terminal leaves lanceolate, entire. Inflorescences 10-12-flowered verticillasters, in terminal, compact spikes. Flowers sessile. Calyx 10-15 mm long, cam-panulate with lanceolate teeth. Corolla 2-lipped, lilac. Fruits dark-brown nutlets. 

A stepwise procedure is used when calculating a dose for an individual patient. First, the limits of the initial tumor and mediastinal lymphadenopathy involved are outlined on chest films taking into account radiologic, bronchoscopic, and clinical information. Second, the target volume is drawn on simulator films. Third, safety margins of the anterior and posterior and lateral or oblique fields are measured (the distance between the target volume and the border of the fields). 

The spectral content of alkenone record has only been assessed in a few records. In one noteworthy example, Schneider et al. (1999) provide evidence that tropical Atlantic SST has a strong imprint from the precessional (—21 kyr) cycle of insolation. Precessional variability drives contrasts in summer and winter heating, particularly at low latitudes. An expected result is that precession regulates the monsoonal cycle of the tropics. This result is consistent with the strength of precession and the weakness of obliquity (41 kyr) components in the spectra of equatorial U f7 records. Both Schneider et al. (1999) and our own unpublished work off the California margin also show that the 41 kyr component in SST is larger at higher latitudes in late Pleistocene time series than it is in low-latitude records. 

Sproli, K.B. 1980. New Zealand and oblique-slip margins Tectonic development up to and during the Cenozoic. In Sedimentation in Oblique-Slip Mobile Zones, Ballance, PP, and Reading, G.H., eds., International Association of Sedomentologists, Special Publication 4, pp. 147-170. 

Fig. 7.1. a Pseudofractures of the epiphyseal ossification centres (arrows). The curved epiphyseal plates of the middle phalanges are superimposed on the secondary ossification centres at their bases producing an effect simulating fractures at the lateral margins, b Overlapping soft tissues of the fingers simulate oblique fractures in a child... 

This is the least severe type of injury pattern with internal rotation of the innominate bone which pivots on the anterior margin of the sacroiliac joint. There may be compression fractures of the sacrum. Pubic rami fractures are common and typically have a known oblique orientation but can be comminuted, compared with the vertical fractures of AP compression injuries (Figs. 12.10,12.11). 

Medial marginal (vertical) fractures in children may traverse the entire thickness of bone or maybe a medial tangential osteochondral fracture. These longitudinal orientated fractures may only be visible on an axial or oblique radiograph. Lateral vertical fractures can occur in athletes due to the pull of the vastus lateralis muscle. 

Fig. 16.5. a AP view showing the alignment of the second metatarsal with the medial margin of the medial cuneiform, b An oblique view showing the alignment of the medial margin of the third metatarsal with the medial margin of the lateral cuneiform... 

Fig. 21.5a-c. Axial oblique MPR (a) showing normal retroperitoneal fat, corresponding to the retroperitoneal pancreatic margin, next to the superior mesenteric artery in the coronal oblique MIP image (b) it is instead possible to appreciate an abnormal density of the fat tissue, suspected for microinfiltration the VR 3D image (c) shows the tumoral invasion of the retroperitoneum... 

Finally, Pseudoleskeella serpentinensis was found within this clade in all analyses. This species differs from other Pseudoleskeella species in being bigger and having thick-walled cells arranged in more or less firm oblique rows, reminiscent of Neckeraceae. The leaf margin of P. serpentinensis is also remotely but quite prominently serrate, a character never found in other species of Pseudoleskeella, but characteristic of both Neckeraceae and Heterocladium. Thus, the placement of P. serpentinensis in Heterocladium or near it seems more likely than in Pseudoleskeella. 

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