Evolution of alkalic lavas at Haleakala Volcano,east Maui,Hawaii     

C. -Y. Chen  F. A. Frey  M. O. Garcia 《Contributions to Mineralogy and Petrology》1990,105(2):197-218

The postshield and posterosional stages of Haleakala Volcano contain intercalated alkalic basalt and evolved alkalic lavas. Isotopic and incompatible element abundance ratios in the Haleakala postshield basalts changed systematically with time, providing evidence for significant temporal changes in the mantle components contributing to the magmatic sources. Specifically, a depleted, i.e. low⁸⁷Sr/⁸⁶Sr and high¹⁴³Nd/¹⁴⁴Nd, mantle component is more abundant in younger lavas. However, as magma-production rates decreased during the postshield and posterosional stages, basaltic melts in magma reservoirs cooled and fractionated, leading to evolved residual melts such as hawaiite. Because primary basalt compositions changed with time, the evolved Haleakala lavas formed from a range of parental compositions. However, basalts and evolved lavas of similar age and isotopic ratios (Sr and Nd) have major and trace element contents that are consistent with a crystal-fractionation model. Although alkalic basalt and hawaiite are the dominant lavas of the postshield stages of both Haleakala and Mauna Kea volcanoes, there are important differences between their lavas. For example, compositional differences between the hawaiite suites at Haleakala and Mauna Kea indicate that, on average, the evolved lavas at Haleakala formed at lower pressures. Also, at Haleakala basalts are intercalated with hawaiites, whereas at Mauna Kea basalts and hawaiites are separated by a sharp boundary. These differences probably reflect a higher magma supply rate to the Haleakala volcano.  相似文献   

On the phase transformation proto- to clino-/orthoenstatite: Neutron powder investigation     

H. Schrader  H. Boysen  F. Frey  P. Convert 《Physics and Chemistry of Minerals》1990,17(5):409-415

The phase transformation proto- to coexisting ortho- and clino-enstatite has been studied by in-situ neutron powder diffraction with samples from Bamble/ Norway. The evolution with temperature was followed in two subsequent cycles with different cooling rates. Refined structural parameters did not indicate any significant anomalies. The transformation behaviour is different for proto to clino (rapid) and the proto to ortho inversion (sluggish). The latter proceeds in two steps: ortho-enstatite starts to grow slowly below 1180 K on cooling, whereas the main transformation takes place below 800 K simultaneously with the proto-clino inversion. The athermal martensitic character is confirmed for the proto to clino inversion. The diffuse background in the powder diagrams is related to stacking faults which are irreversibly created during the transformation and affect the degree of order.Work supported by funds of the BMFT under 03-SC1LMU  相似文献   

Latent and sensible heat flux predictions from a uniform pine forest using surface renewal and flux variance methods   总被引：1，自引：0，他引：1  

Gabriel Katul  Cheng-I Hsieh  Ram Oren  David Ellsworth  Nathan Phillips 《Boundary-Layer Meteorology》1996,80(3):249-282

A surface renewal model that links organized eddy motion to the latent and sensible heat fluxes is tested with eddy correlation measurements carried out in a 13m tall uniform Loblolly pine plantation in Duke Forest, Durham, North Carolina. The surface renewal model is based on the occurance of ramp-like patterns in the scalar concentration measurements. To extract such ramp-like patterns from Eulerian scalar concentration measurements, a newly proposed time-frequency filtering scheme is developed and tested. The time-domain filtering is carried out using compactly-supported orthonormal wavelets in conjunction with the Universal Wavelet Thresholding approach of Donoho and Johnstone, while the frequency filtering is carried out by a band-pass sine filter centered around the ramp-occurrence frequency as proposed by other studies. The method was separately tested for heat and water vapour with good agreement between eddy correlation flux measurements and model predictions. The usefulness of the flux-variance method to predict sensible and latent heat fluxes is also considered. Our measurements suggest that the simple flux-variance method reproduces the measured heat and momentum fluxes despite the fact that the variances were measured within the roughness sublayer and not in the surface layer. Central to the predictions of water vapour fluxes using the flux-variance approach is the similarity between heat and water vapour transport by the turbulent air flow. This assumption is also investigated for this uniform forest terrain.  相似文献   

Immigration impacts on internal migration of the poor: 1990 census evidence for U.S. states     

Frey WH 《International journal of population geography : IJPG》1995,1(1):51-67

"This article presents newly-available migration data from the 1990 U.S. census to assess immigration and internal migration components as they affect state poverty populations. New immigrant waves are heavily focused on only a few 'port-of-entry' states. It is suggested that these immigrants have begun to impact upon internal migration into and out of these 'high immigration states', and have also altered the national system of internal migration patterns. This article addresses three questions: How do the magnitudes of poverty population out-migration from high immigration states compare with those of other states? Is this out-migration selective on particular social and demographic groups? Is immigration a significant determinant of internal migration of the poor population? The results of this analysis are consistent with the view that recent, focused immigration is associated with out-migration among a state's poor longer-term residents."  相似文献   

An experimental study of the partitioning of a rare earth element (Gd) in the system diopside—aqueous vapour     

Robert A. Zielinski  Frederick A. Frey 《Geochimica et cosmochimica acta》1974,38(4):545-565

The partitioning of Gd in the experimental system diopside-aqueous vapor as a function of temperature, pressure, composition of the phases, time, grain size, solid-liquid ratio and Gd concentration has been investigated. A radioactive tracer measurement was used to determine Gd concentration in the separated phases. Diposides were reacted with aqueous vapor containing tracer Gd and reversibility was tested by reacting Gd-doped diopsides with pure aqueous vapor. Equilibration of Gd between the bulk of the diopside and the liquid was found to be limited by the slow rate of Gd diffusion in diopside, maximum value of D = 2 × 10^?15cm²sec^?1 at 800°C and 1 kb. Depending on whether the diopside was previously synthesized or synthesized from an oxide mix during the experiment, Gd concentrations were zoned in the crystal such that higher concentrations existed at the edges or center, respectively. Equilibrium is difficult to achieve in these experiments, but at the optimum experimental conditions for equilibration, the Gd diopside-aqueous vapor distribution coefficient is 20 ± 6 (800°C, 1 kb) in approximate agreement with previous results of 55 ± 23. Changing the composition of the aqueous vapor indicated that possible mechanisms for Gd substitution included coupling of Gd³⁺ with H⁺ or Na⁺ replacing 2Ca²⁺, or substitution of 2Gd³⁺ for 3Ca²⁺ with formation of a cation vacancy.  相似文献   

Post-eclipse brightening and non-brightening of Io     

Herbert Frey 《Icarus》1975,25(3):439-446

It may be possible to understand the apparent intermittent nature of the post-eclipse brightenings and nonbrightenings of Io in terms of a nonuniform distribution of blue reflectors grouped in the hemisphere centered at 0° longitude. The dimensions required for such blue mirrors are consistent with very large craters. The high blue albedo of water frost and other ices makes these materials likely candidates for the reflectors.  相似文献   

Evolution of Icelandic central volcanoes: evidence from the Austurhorn intrusion,southeastern Iceland     

Tanya Furman  Peter S Meyer  Fred Frey 《Bulletin of Volcanology》1992,55(1-2):45-62

The Austurhorn intrusive complex in southeastern Iceland represents an exhumed Tertiary central volcano. The geometry of the intrusion and geochemistry of the mafic and felsic rocks indicate Austurhorn was a volcanic center analogous to Eyjafjallajökull and Torfajökull in Iceland's eastern neovolcanic zone (EVZ). Early transitional tholeiitic basalt magmatism at Austurhorn formed a shallow crustal chamber 5 km in diameter. Apparent rhythmic modal layering of, and intrusive contacts within, the gabbro indicate the mafic chamber was replenished frequently as it cooled and crystallized. Felsic activity postdated near-solidification of the gabbro; numerous granitic magmas intruded along gabbro margins and within the adjacent crust. Field relations indicate that infrequent felsic replenishment prevented convective mixing of the Austurhorn chamber during this time, although commingled mafic and felsic magmas are observed in an extensive net veined complex. Late stage mafic dikes intrude the entire complex, suggesting that magmatic heat was abundantly available throughout the evolution of the Austurhorn system. Plagioclase and clinopyroxene compositions in mafic through felsic rocks, including gabbros, support a model of progressive differentiation. Field relations constrain the felsic magmas to originate at P1 kbar, presumably by fractional crystallization. The structure and geochemistry of the Austurhorn intrusive complex suggest formation in an immature rift environment similar to the modern EVZ. The proposed rift segment was parallel to the western and eastern neovolcanic zones, and probably resulted from a reorganization of plate boundaries 7 Ma (Saemundsson 1979; Helgason 1985; Jancin et al. 1985) triggered by activity of the Iceland mantle plume.  相似文献   

On the proto- to ortho-/clino enstatite phase transformation: Single crystal X-ray and inelastic neutron investigation     

H. Boysen  F. Frey  H. Schrader  G. Eckold 《Physics and Chemistry of Minerals》1991,17(7):629-635

High temperature X-ray investigations of enstatite from Bamble shows that the proto (PE) to ortho (OE)/clino (CE) inversion is most probably triggered by preformed single stacking faults acting as nuclei and completed by a subsequent rapid growth process compatible with the martensitic nature of the transformation. New stacking faults are created during the transformation. From a detailed analysis of line profiles we deduce the formation of out-of-phase OE domains which are intergrown with well ordered CE sequences. Single layer faults and PE type faults can be ruled out. A transformation mechanism similar to that proposed by Sadanaga et al. (1969) fits well with our results. Inelastic neutron scattering experiments show that the origin of the transformation is not an elastic shear instability. A transient increase of the elastic constant c ₅₅ is interpreted as a secondary effect caused by elastic strains in the progress of the transformation.Work was supported by the BMFT under 03-SC1LMU3  相似文献   

The Chan Hol cave near Tulum (Quintana Roo,Mexico): evidence for long‐lasting human presence during the early to middle Holocene          下载免费PDF全文

Fabio Hering  Wolfgang Stinnesbeck  Jens Folmeister  Eberhard Frey  Sarah Stinnesbeck  Jerónimo Avilés  Eugenio Aceves Núñez  Arturo González  Alejandro Terrazas Mata  Martha Elena Benavente  Carmen Rojas  Adriana Velázquez Morlet  Norbert Frank  Patrick Zell  Julia Becker 《第四纪科学杂志》2018,33(4):444-454

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Limnological instrumentation in the middle of the 19th century: the first temperature and density profiles measured in the Dead Sea     

Aharon Oren 《中国海洋湖沼学报》2015,33(6):1496-1504

The first modern survey of the Dead Sea was performed by the Geological Survey of Israel in 1959–1960,and the report published remains the baseline study for our understanding of the physical and chemical properties of the lake.At the time the Dead Sea was a meromictic lake with a strong salinity gradient separating the deep waters(40 m depth) from the less saline surface waters.A few results of analyses of deeper water samples collected in the 1930 s were reported,but overall we have very little information about the structure of the lake's water column before the 1959–1960 survey.However,it is little known that data on the physical and the chemical structure of the Dead Sea water column were obtained already in the middle of the 19 th century,and the information collected then is highly relevant for the reconstruction of the limnological properties of the lake in earlier times.The expedition of Lieutenant William Lynch(U.S.Navy) in 1848 reported the presence of a temperature minimum at a depth of ~18 m,and also retrieved a water sample collected close to the bottom for chemical analysis.In 1864,the French Dead Sea exploration by the Duc de Luynes and his crew yielded detailed density and salinity profiles for a number of sampling stations.The results of these pioneering studies are discussed here,as well as the sampling equipment and measuring instruments used by the 1848 and the 1864 expeditions.  相似文献