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These tectonic events involved the emplacement of a number of thrust sheets, each of which was emplaced from NE to SW onto the Oman Tethyan continental margin which had been rifted during the Permian to Late Triassic – Early Jurassic(Robertson and Searle 1990).
Between the 5th and 4th millennia BP, a rocky profile with a wave-cut platform cutting across pyroclastites emplaced from the surrounding volcanoes was predominant in the coastal landscape.
The Campanian Ignimbrite succession is formed by a basal plinian pumice fall deposit, overlain by a complex architecture of pyroclastic density current deposits emplaced from a single sustained pyroclastic density current through a mechanism of vertical and lateral accretion.
Moore says the jury is still out on whether Tombaugh Regio was emplaced from below or shaped from above.
The techniques of stress relief mining in low-permeability coal seams, pillarless mining, and Y-type ventilation systems emplaced from gob side retained roadways have been developed and applied successfully to control these gas accidents (Yuan 2008b, 2009).
The distal part of the delta consists of marine shales which are characteristically overpressurized and hydrocarbons are emplaced from the marine shales into reservoir by episodic charging due to dissipation of overpressure via fracturing, healing of the fractures and refracturing (Tuttle et al. 1999).
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These lavas were initially emplaced far from the incipient trench either in a rear-arc position like the Valu Fa lavas, or in a stretched arc at the termination of a rift like in northern Tonga or in the southern New Hebrides.
Shallow wells were emplaced 3 m from the stream bank (approximately 6 m from center of channel) within the root zone (screened interval 30 60 cm bls).
The oxidation of some "fresh lava" particles (Fig. 7(c)) clearly indicates that they come from emplaced lava which was still hot at or near surface.
The factors leading to drift degradation include stresses from the overburden, stresses induced by the heat released from the emplaced waste, stresses due to seismically related ground motions, and time-dependent strength degradation.
It ultimately split into three lobes that flowed down the three branches of Barranca el Cordobán on the SSW flank of Volcán de Colima; the lava advanced atop previously emplaced pyroclastic-flow deposits from the same eruptive event, whose total volume is estimated as 24×105 m3.
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