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Derivation of A Geomagnetic Model to N = 63 总被引：4，自引：0，他引：4
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Samuel N. Luoma Daniel J. Cain Kay Ho Anne Hutchinson 《Marine environmental research》1983,10(4):209-222
In static toxicity experiments, tolerance to soluble Cu of the bivalve, Macoma balthica, and the copepod, Acartia clausi, varied substantially among populations sampled within San Francisco Bay. Intraspecific tolerance differed ten-fold or more for both species over relatively small distances, suggesting geographical isolation of populations is not a prerequisite for the development of intraspecific differences in tolerance by aquatic organisms. 相似文献
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Partitioning Tracer Tests for Evaluating Remediation Performance 总被引：1，自引：0，他引：1
R. Brent Cain Gwynn R. Johnson John E. McCray William J. Blanford Mark L. Brusseau 《Ground water》2000,38(5):752-761
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Anthony C. Cain 《International Journal of Earth Sciences》1975,64(1):192-216
Highly deformed regionally metamorphosed rocks of the Natal-Namaqua belt north of Durban preserve the features of a major Precambrian geosynclinal sequence, with possible reactivated oceanic and continental floor material. The broad scale grouping of similar lithologies into mappable geologic units is possible. Formation status is assigned to certain units, classified in the Natal group. Variation of lithologic character of these rocks within the belt is correlated with facies of orogenic deposition. Three zones of regional progressive metamorphism are recognised, and the metamorphosed rocks of the belt can be divided into a high-pressure intermediate, intermediate-pressure and intermediate-low pressure facies series types corresponding to the upper-greenschist facies, low-amphibolite facies and middle-amphibolite facies respectively. These three metamorphic terrains display considerable differences in composition and structural style, and correspond to the major tectonic units of the belt. Evidence gained from a study of the distribution of regional metamorphism in the Natal-Namaquarides north of Durban, has reinforced the favourability of applying the theory of plate tectonics to the development of the orogen in an attempt to obtain a broader understanding of the geologic history of the belt. Furthermore, the complex suite of metamorphites and associated intrusive phases constituting the belt involves the deformation and metamorphism of lithological types similar to those described in orogenic belts in other parts of the world. 相似文献