Report of the committee on the nomenclature of faults

Ohne Zusammenfassung

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Report of the committee on the nomenclature of faults

     

Observations des bords brillants dans NGC 281, IC 434 et M 16

Sommaire Les photographies monochromatiques en H, [Nii] 6584 et [Oiii] 5007 ont été obtenues sur NGC 281, IC 434 et M 16 eu vue de la détection et de l'étude des bords brillants. A partir de ces photos, on accède à la carte d'égal rapport [Nii]/H grâce à la méthode décrite par Louise et Sapin (1972). A l'exclusion des bords brillants, ce rapport varie très peu à l'intérieur d'une même nébuleuse. Par contre à l'approche des fronts d'ionisation, il augmente de façon spectaculaire et systématique.Le renforcement de la raie [Oiii] vers les bords brillants suggère la présence des inhomogénéités (globules ou/et filaments) et le rôle possible que jouent les mécanismes d'échange de charges étudiés par Aller et Keyes (1980).

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Observations of bright rims in NGC 281, IC 434 and M 16

Monochromatic plates are obtained in H, [Nii] 6584 and [Oiii] 5007 lines for three Hii regions: NGC 281, IC 434 and M 16. They allow both detection and physical studies of bright rims. Indeed, it is shown that bright rims appear most contrasted on [Nii] and [Oiii] plates. Furthermore, maps of ratio [Nii]/H are derived from the method described by Louise and Sapin (1972). This ratio remains practically constant within the nebula, except for bright rims where it increases. This may be understood by means of both increasing abundanceN(N⁺/N(H⁺) and temperature following to the model of Mallik (1975).The [Oiii] enhancement towards bright rims in M 16 suggests the presence of inhomogeneities (globules or/and filaments) and the possible role played by charge exchange mechanisms as pointed out by Aller and Keyes (1980).

     

Magma mixing in granitic rocks of the central Sierra Nevada,California

The El Capitan alaskite exposed in the North American Wall, Yosemite National Park, was intruded by two sets of mafic dikes that interacted thermally and chemically with the host alaskite. Comparisons of petrographic and compositional data for these dikes and alaskite with published data for Sierra Nevada plutons lead us to suggest that mafic magmas were important in the generation of the Sierra Nevada batholith. Specifically, we conclude that: (1) intrusion of mafic magmas in the lower crust caused partial melting and generation of alaskite (rhyolitic) magmas; (2) interaction between the mafic and felsic magmas lead to the observed linear variation diagrams for major elements; (3) most mafic inclusions in Sierra Nevada plutons represent chilled pillows of mafic magmas, related by fractional crystallization and granitoid assimilation, that dissolve into their felsic host and contaminate it to intermediate (granodioritic) compositions; (4) vesiculation of hydrous mafic magma upon chilling may allow buoyant mafic inclusions and their disaggregation products to collect beneath a pluton's domed ceiling causing the zoning (mafic margins-to-felsic core) that these plutons exhibit.     

The origin of lavas and ignimbrites of the Taupo Volcanic Zone,New Zealand,in the light of oxygen isotope data

The Taupo Volcanic Zone consists predominantly of andesites at each end and about a 20times larger volume of rhyolites (incl. ignimbrites and pumice) in the center. In a δ¹⁸O vs SiO₂ diagram the rhyolites do not continue the increasingly ¹⁸O-contaminated andesite (basalt to dacite) trend, but have lower δ¹⁸O values than the most differentiated andesites. Comparison with δ¹⁸O of greywackes and conjectural granitoids seems to rule out a partial fusion origin. In retrospect the Sr isotope data of Ewart and Stipp (1968) are seen to confirm this conclusion. Isotopic adjustment of source rocks before partial fusion, by exchange with circulating subsurface waters, is highly unlikely because of the combined demands for O and Sr isotope shifts, and the constraint offered by the normal igneous to somewhat enriched δ¹⁸O values of the rhyolites. Oxygen isotope results confirm separate origins or at least different modes of ascent of basalt and andesites on one hand and rhyolites on the other. Both magma types appear to have originated below crustal formations and both have become contaminated by greywacke through which they passed to reach the surface.     

Radium in the near-surface Caribbean Sea

Recent radium measurements from the near-surface Caribbean Sea are presented. The surface horizontal and vertical distributions of²²⁶Ra are essentially the same as reported by Szabo et al. (1967) for the early 1960's. The²²⁶Ra activity at the surface is relatively uniform across the Caribbean, with an average of8.2±0.4dpm/100kg. The subsurface distribution to ～200 m averages7.8±0.4dpm/100kg and increases slowly below 200 m. reaching ～9.5 dpm/100 kg at 560 m. In contrast to²²⁶Ra, the surface concentration of²²⁸Ra was much more variable in both time and space. An average increase of 33% was found between 1968 and 1976 in the western Caribbean and during both years an anomalously high²²⁸Ra activity was found in the eastern Caribbean. These data support previous hypotheses that water entering the eastern Caribbean has been enriched in²²⁸Ra prior to entry and that variable mixing of the Atlantic water masses found to the northeast and southeast of the Lesser Antilles may produce temporal variations in the near-surface²²⁸Ra activity. Scatter plots of²²⁸Ra vs. salinity and sigma-t indicate that the near-surface vertical distribution of²²⁸Ra in the Caribbean Sea is predominantly influenced by advection. Thus²²⁸Ra cannot be used to study near-surface vertical mixing rates in this region.     

Origin of Sierra Nevadan granite: evidence from small scale composite dikes

Composite dikes at Hell Hole Meadow, in the central Sierra Nevada, contain hybrids created by small scale mixing of andesitic and rhyolitic magmas. Early rhyolitic injections had partially solidified when subsequent andesitic magmas arrived and mixed with small increments of remnant rhyolitic magma. In major element chemistry, the hybrid rocks define linear MgO-variation diagrams that closely resemble those for the Half Dome, Mt. Givens, and Eagle Peak granodiorites. The patterns suggest that mixing of mafic and felsic magmas has been important in the evolution of these plutons.Hornblendes in three Hell Hole Meadow hybrid rocks ranging from dacite to andesite display indistinguishable crystal-chemical variation patterns. The crystals apparently developed as phenocrysts of endmember andesitic magma prior to the mixing event and retained their compositional character in the hybridization event. Plutonic hornblendes (Dodge et al. 1968; Noyes et al. 1983) display crystal-chemical patterns nearly identical to those in the dike cores making it unlikely that the plutonic hornblendes represent restite of a complex lower crust.Hornblende chemical data from a suite of rocks collected across the width of the compositionally zoned Half Dome granodiorite (Yosemite National Park) define clusters, like their Hell Hole Meadow counterparts, that are very similar to one another despite the large range in host rock bulk composition. Sr isotopic data (Kistler et al. 1986) and linear MgO-variation patterns for the major elements (Reid et al. 1983) suggest that the Half Dome is a mixture of high-alumina basalt and rhyolitic magmas. We propose that while the bulk chemistry of hybrid granodiorites is determined by the proportions of the constituent mafic and felsic magmas, the hornblendes in the mixed rocks largely retain compositions created in the mafic component prior to mixing. Mixing may occur either by incremental addition of felsic magma into a relatively large volume of mafic magma (as at Hell Hole Meadow), or by the chilling and subsequent disaggregation of mafic pillows in a largely felsic host.     

On climatic analogs in paleoclimatic reconstruction

Many of the problems that have been discussed with regard to the analog approach to paleoclimatic reconstruction may be illustrated by consideration of basic principles and definitions, and the logical consquences thereof. Specific attention is directed toward the definition of the regional macroclimate as the modal microclimate and to a series of axioms: (1) There are various microclimates which depart more or less from the macroclimate in each terrestrial region. (2) Environment and climate change on time scales from near instantaneous to millions of years. (3) Climate is multidimensional (a vector), not a single scalar datum. (4) Biotic assemblage changes in response to environmental (including climatic) changes are expressed primarily in terms of reproductive success. One may conclude from the corollaries to these axioms that perfect analogs cannot be found for any Holocene climate, but that “partial analogs” (“transfer equations”) may still be used if allowance is made for shared variance.     

Computer reliability analysis of coal-cleaning distribution curves

Three types of distribution curve error are defined, i.e., the fitting deviation, the real deviation and the test error. Since the absolute distribution curve is never known, both the real deviation and the test error are unknown. Only the fitting deviation can be calculated and is a measure of the difference between a calculated distribution curve and the experimental data. However, the real deviation is of primary importance in evaluating the reliability of calculated distribution curves. This paper uses a microcomputer to simulate absolute distribution curves and obtains numerical relationships between the real deviation, the fitting deviation and the test error.More than 500 tests using a microcomputer show that a relationship exists between the fitting deviation, test error and real deviation. In most cases, the fitting deviation and the real deviation are close to each other. Both the fitting and the real deviation are smaller than the test error if the selected model is suitable.     

The occurrence and behavior of radium in saline formation water of the U.S. Gulf Coast region

Radium has been measured in deep saline formation waters produced from a variety of U.S. Gulf Coast subsurface environments, including oil reservoirs, gas reservoirs and water-producing geopressured aquifers. A strong positive correlation has been found between formation-water salinity and Ra activity, resulting from the interaction of formation water with aquifer matrix. Ra isotopes enter the fluid phase after being produced by the decay of parent elements U and Th, which are located at sites on and within the solid matrix.Processes that are belived to be primarily responsible for transferring Ra from matrix to formation water are chemical leaching and alpha-particle recoil. Factors controlling the observed salinity—Ra relationship may be one or a combination of the following factors: (a) ion exchange; (b) increased solubility of matrix silica surrounding Ra atoms, coupled with a salinity-controlled rate of reequilibration of silica between solution and quartz grains; and (c) the equilibration of Ra in solution with detrial barite within the aquifer.No difference was found in the brine-Ra relation in water produced from oil or gas wells and water produced from wells penetrating only water-bearing aquifers, although the relation was more highly correlated for water-bearing aquifers than hydrocarbon-containing reservoirs.     

Coexisting bronzite and clinobronzite and the thermal evolution of the Steinbach meteorite

Steinbach is a stony-iron meteorite with approximately equal amounts of silicate and metal that shows Widmanstätten structure. The silicate portion contains tridymite, orthobronzite, and clinobronzite that formed by inversion from high-temperature protobronzite. The assemblage orthobronzite-protobronzite-tridymite-metallic iron indicates an equilibrium temperature of 1200°C and an ?o₂ of 10^?12 under a total pressure of less than 2 kbar. Preservation of the high-temperature phase relations implies much more rapid cooling in the 1200-700°C range than the rates that have been deduced for the development of Widmanstätten structure in the 700-500°C range.