Possible premonitory strain changes associated with an earthquake swarm near Mina,Nevada     

Keith F. Priestley 《Pure and Applied Geophysics》1975,113(1):251-256

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Flow patterns in the Northwest African upwelling area     

Dr. E. Mittelstaedt  Dr. D. Pillsbury  Dr. R. L. Smith 《Ocean Dynamics》1975,28(4):145-167

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A comparison of the recent eruptions of Mt. Pelée,Martinique and Soufrière,St. Vincent     

M. J. Roobol  A. L. Smith 《Bulletin of Volcanology》1975,39(2):214-240

The simultaneous eruption of Mt. Pelée, Martinique and Soufrière, St. Vincent are regarded as the first recognized examples of Pelean-type and St. Vincent-type pyroclastic eruptions. Both produced nuées ardentes, the former usually laterally directed because of the presence of a dome and the latter vertically directed from an open crater. Both volcanoes have subsequently erupted for a second time this century. The 1902–05 and 1929–32 eruptions of Mt. Pelée produced andesite lava of almost identical composition and mineralogy. Both contain two generations of plagioclase, orthopyroxene, Fe-Ti oxide, corroded brown amphibole and olivine rimmed by pyroxene. In contrast, the Soufrière material is more basic in composition varying from basaltic andesite to basalt in 1902–03 and basaltic andesite in 1971–72. The Soufrière material contains two generations of plagioclase (with those of 1971–72 having additional zones of labradorite), clinopyroxene, orthopyroxene, olivine and Fe-Ti oxide. The pyroclastic deposits are strikingly different, those from the Pelean-type eruption are termed «block and ash deposits» being characterised by poorly vesicular lava blocks up to 7 m in diameter, while the St. Vincent-type eruption produced «scoria and ash deposits» containing vesicular ropey blocks or bombs no larger than 1 m in diameter. The differences in styles of eruption are attributed to differences in viscosity and mechanism of eruption of the magmas. Stratigraphic studies of Mt. Pelée reveal that the volcano has produced basaltic andesite scoria and ash deposits from St. Vincent-type eruptions. It is concluded that the recent eruptions of Pelée tapped a deep level magma during both eruptions releasing magma of similar composition, while the 1971 Soufrière magma is thought to be a remnant of the 1903 basaltic magma which remained at a high level within the volcano where it underwent enrichment in plagioclase and loss of olivine and oxide.  相似文献   

The McArthur deposit: A review of the current situation     

N. J. W. Croxford  B. L. Gulson  J. W. Smith 《Mineralium Deposita》1975,10(4):302-304

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Experimental studies of sodic microperthites from the Loch Ailsh syenite     

Ian Parsons  Peter Smith 《Lithos》1974,7(4):217-225

Solvus curves under both ‘dry’ and ‘hydrothermal’ (P_H2O = 1 kbar) conditions have been determined for two microperthitic alkali feldspar starting materials from the Loch Ailsh syenite complex, Assynt, Scotland. One sample (Ab₇₄ Or₂₄ An₂) possessed a K-phase showing dominant monoclinic symmetry to both powder and single-crystal X-ray methods, the other (Ab₈₈Or₃₀An₂) had maximum microcline as K-phase. These materials gave essentially identical solvi for both types of experiment, interpreted as indicating similar degrees of local order in the K-phase, but with differing domain size, leading to the different X-ray properties. The ‘dry’ solvus curves confirm the determination of the microcline-low albite solvus of Bachinski & Müller. The hydrothermal curves are used to estimate P_H1O <3.5 kbars, T > 755 °C for emplacement of the Loch Ailsh syenites.  相似文献   

On the chemical composition of atmospheric aerosols — Part II: Trends between some chemical components of rainwater and physical variables over the United States     

Henry M. Papée  A. Cormac Smith 《Pure and Applied Geophysics》1959,44(1):204-215

Summary Annual average results of rainwater analysis, carried out byC. Junge at about 60 stations of the United States sampling network are used in an attempt to correlate the ionic species present in rain, as a general contribution to atmospheric chemicstry. Correlation with physical parameters is attempted at the same time in some cases, and the resulting trends discussed. The results obtained are presented in the general form of linear and planar correlation, and linear regression coefficients.  相似文献   

Quaternary lavas from the southern Cascades,western U.S.A.     

A. L. Smith  I. S. E. Carmichael 《Contributions to Mineralogy and Petrology》1968,19(3):212-238

A series of basaltic and andesitic lavas from three centers in the Cascades (Lassen, Medicine Lake, Mt. Shasta) have been investigated. The lavas are weakly porphyritic, containing phenocrysts of plagioclase, augite, and olivine or orthopyroxene; these phases are also found in the groundmass. Titanomagnetite is a groundmass phase in most lavas but it appears to be absent in some. A sub-calcic augite is found in the groundmass in some of the basic lavas. Orthopyroxenes are present only in the salic lavas and show an increase in calcium with increasing iron. The range in composition shown by both phenocryst and groundmass plagioclase is very similar except that the phenocrysts extend to slightly more calcic compositions. The residual glasses in many of the lavas have a rhyolitic composition. However, only those from the Shasta andesites have normative salic constituents that plot near the ternary minimum in the Ab-Or-Qtz system at 500 bars. Both chemical and mineralogical data allow the lavas of the different centers to be distinguished from one another. The most likely origin for the orogenic lavas of the Cascades is by partial melting of the upper mantle.  相似文献   

Petroleum tankship safety: by R. C. Page and A. Ward Gardner. 1971. London: Maritime Press. viii + 210 pp. Price £1.50     

J. Wardley Smith 《Marine pollution bulletin》1972

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Finite strip analysis of the dynamic response of beam and slab highway bridges     

J. W. Smith 《地震工程与结构动力学》1972,1(4):357-370

This paper presents a method of analysis for the dynamic response of a simply supported beam and slab bridge under the action of a moving vehicle. The bridge is idealized as an orthotropic plate and, in the analysis, is subdivided into a number of finite strips. The vehicle is idealized as a moving sprung mass. Viscous damping is taken into account for both bridge and vehicle. The results show that there is significant variation of response across transverse sections of the bridge. Furthermore the dynamic magnification is considerably greater than that predicted by a more approximate method in which the bridge is idealized as a simple prismatic beam.  相似文献   

Nitrous oxide emission from Gulf Coast wetlands     

C.J. Smith  R.D. DeLaune  W.H. Patrick 《Geochimica et cosmochimica acta》1983,47(10):1805-1814

Nitrous oxide evolution may contribute to partial destruction of the ozone layer in the stratosphere. A two year study of the release of N₂O from adjoining salt, brackish, and fresh marsh sediment indicates that the annual emission was 31, 48, and 55 mg N m^?2 respectively. Emission from open water area was less than the corresponding emission from the marsh sediment. In vitro experiments indicate that the N₂O emission was increased when the sediment was drained for extended periods of time. The addition of NO₃^? significantly increased the rate of N₂O evolution, indicating that a large potential for denitrification exists in the anoxic sediment. Appreciable losses of N₂O would only be expected when the marshes receive an extraneous source of nitrate such as sewage and/or wastewater.The contribution of the Gulf Coast wetlands to the atmospheric N₂O balance is estimated to be 3.3 × 10⁹ g N₂O. The maximum average daily emission was equivalent to 1.5 g N₂O-N ha^?1, which is less than the measured emission from uncultivated soils (Mosieret al., 1981) but greater than the estimates from noncropped land (CAST, 1976).  相似文献