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排序方式: 共有249条查询结果,搜索用时 15 毫秒
81.
Volker Stähle Rainer Altherr Lutz Nasdala Thomas Ludwig 《Contributions to Mineralogy and Petrology》2011,161(2):275-291
Shock veins up to 1.1 mm thick were found within non-porous lithic clasts from suevite breccia of the Nördlinger Ries impact structure. These veins were studied by optical microscopy in transmitted and reflected light and by scanning electron microscopy. In shocked amphibolites, two types of Ca-rich majorite occur within and adjacent to the veins. The first type crystallized from shock-induced melts within the veins. Si contents of these majorites suggest dynamic pressure of ~15–17 GPa, implying minimum temperatures in the range of ~2,150–2,230°C. The second type of majorite was formed adjacent to the shock veins within pargasitic hornblende. This majorite contains significant amounts of H2O (0.7–0.9 wt%). Based on the textural setting, the shrinkage cracks and the chemical compositions of both phases, a solid-state mechanism is deduced for the hornblende to majorite phase transition. Both genetic types of Ca-rich majorite are described for the first time from a terrestrial impact crater. Along with stishovite, majorite constitutes the second silicate mineral displaying sixfold coordination of Si at Ries. Using micro-Raman spectroscopy, jadeite + coesite and jadeite + grossular were identified within local melt glasses of alkali feldspar and plagioclase composition, respectively. Stishovite aggregates, produced by solid-state reaction, along with shock-induced high-pressure melt glasses of almandine composition were also detected in shock veins of a garnet-cordierite-sillimanite restite. The quenched, homogeneous almandine glasses point to melting temperatures of more than ~2,500°C for the veins. Our findings demonstrate that terrestrial shock veins can give valuable information on shock-induced mineral transformations and transient high pressures of host rocks during a natural impact event. 相似文献
82.
Environmental controls on stable isotope precipitation values over Mali and Niger,West Africa 总被引:2,自引:0,他引:2
This study evaluated the effects of the environmental factors precipitation amount (P), temperature (T), and vapor pressure (V
p) on the stable isotope composition (δ) of precipitation and the excess-deuterium (d) parameter in Mali and Niger, West Africa. At both locations, δ values were greatly affected by seasonal climatic conditions and a statistically significant negative correlation was observed
between δ and P. In Mali, a statistically significant negative correlation was also observed between δ and V
p. There was no statistically significant correlation between δ and T. Mean-weighting of δ values may be masking both dry-season and individual storm event precipitation phenomena, which are otherwise observed in
arithmetically averaged δ values. Mean monthly d values for peak monsoonal months indicate that precipitation is first-fraction, gaining little recycled water on its journey
inland from the Atlantic Ocean near the equator. Agreement between rainy-season precipitation and groundwater δ values, specifically peak monsoonal months, indicates that groundwater is being recharged by infiltration of current monsoonal
rains and is not paleo-groundwater recharged under past climatic conditions. Similarity between rainy-season precipitation
and groundwater d values provide another indication that monsoonal precipitation under current climatic conditions is the source of groundwater
recharge. The knowledge that groundwater is recently recharged monsoonal rains, rather than paleo-groundwater, is important
for evaluating groundwater sustainability and the effects that climate change will have on water resources. Understanding
and predicting changes in precipitation amounts and intensities, which ultimately affect timing and amount of groundwater
recharge, is critical for water resource management. 相似文献
83.
Dieter Stffler Natalya A. Artemieva Boris A. Ivanov Lutz Hecht Thomas Kenkmann Ralf Thomas Schmitt Roald Alberto Tagle Axel Wittmann 《Meteoritics & planetary science》2004,39(7):1035-1067
We present and interpret results of petrographic, mineralogical, and chemical analyses of the 1511 m deep ICDP Yaxcopoil‐1 (Yax‐1) drill core, with special emphasis on the impactite units. Using numerical model calculations of the formation, excavation, and dynamic modification of the Chicxulub crater, constrained by laboratory data, a model of the origin and emplacement of the impact formations of Yax‐1 and of the impact structure as a whole is derived. The lower part of Yax‐1 is formed by displaced Cretaceous target rocks (610 m thick), while the upper part comprises six suevite‐type allochthonous breccia units (100 m thick). From the texture and composition of these lithological units and from numerical model calculations, we were able to link the seven distinct impact‐induced units of Yax‐1 to the corresponding successive phases of the crater formation and modification, which are as follows: 1) transient cavity formation including displacement and deposition of Cretaceous “megablocks;” 2) ground surging and mixing of impact melt and lithic clasts at the base of the ejecta curtain and deposition of the lower suevite right after the formation of the transient cavity; 3) deposition of a thin veneer of melt on top of the lower suevite and lateral transport and brecciation of this melt toward the end of the collapse of the transient cavity (brecciated impact melt rock); 4) collapse of the ejecta plume and deposition of fall‐back material from the lower part of the ejecta plume to form the middle suevite near the end of the dynamic crater modification; 5) continued collapse of the ejecta plume and deposition of the upper suevite; 6) late phase of the collapse and deposition of the lower sorted suevite after interaction with the inward flowing atmosphere; 7) final phase of fall‐back from the highest part of the ejecta plume and settling of melt and solid particles through the reestablished atmosphere to form the upper sorted suevite; and 8) return of the ocean into the crater after some time and minor reworking of the uppermost suevite under aquatic conditions. Our results are compatible with: a) 180 km and 100 km for the diameters of the final crater and the transient cavity of Chicxulub, respectively, as previously proposed by several authors, and b) the interpretation of Chicxulub as a peak‐ring impact basin that is at the transition to a multi‐ring basin. 相似文献
84.
Matthias EBERT Lutz HECHT Alexander DEUTSCH Thomas KENKMANN 《Meteoritics & planetary science》2013,48(1):134-149
Abstract– In the context of the MEMIN project, a hypervelocity cratering experiment has been performed using a sphere of the iron meteorite Campo del Cielo as projectile accelerated to 4.56 km s?1, and a block of Seeberger sandstone as target material. The ejecta, collected in a newly designed catcher, are represented by (1) weakly deformed, (2) highly deformed, and (3) highly shocked material. The latter shows shock‐metamorphic features such as planar deformation features (PDF) in quartz, formation of diaplectic quartz glass, partial melting of the sandstone, and partially molten projectile, mixed mechanically and chemically with target melt. During mixing of projectile and target melts, the Fe of the projectile is preferentially partitioned into target melt to a greater degree than Ni and Co yielding a Fe/Ni that is generally higher than Fe/Ni in the projectile. This fractionation results from the differing siderophile properties, specifically from differences in reactivity of Fe, Ni, and Co with oxygen during projectile‐target interaction. Projectile matter was also detected in shocked quartz grains. The average Fe/Ni of quartz with PDF (about 20) and of silica glasses (about 24) are in contrast to the average sandstone ratio (about 422), but resembles the Fe/Ni‐ratio of the projectile (about 14). We briefly discuss possible reasons of projectile melting and vaporization in the experiment, in which the calculated maximum shock pressure does not exceed 55 GPa. 相似文献
85.
86.
87.
Hajnalka Breuer Ferenc ács Borbála Laza ákos Horváth István Matyasovszky Kálmán Rajkai 《Theoretical and Applied Climatology》2012,109(3-4):577-590
The effects of two soil datasets on planetary boundary layer (PBL) height are analyzed, using model simulations. Simulations are performed with the MM5 weather prediction system over the Carpathian Basin, with 6?km horizontal resolution, investigating three summer days, two autumn, and one winter day of similar synoptic conditions. Two soil datasets include that of the United States Department of Agriculture, which is globally used, and a regional Hungarian called Hungarian unsaturated soil database. It is shown that some hydraulic parameter values between the two datasets can differ up to 5–50%. These differences resulted in 10% deviations in the space–time-averaged PBL height (averaged over Hungary and over 12?h in the daytime period). Over smaller areas, these relative deviations could reach 25%. Daytime course changes in the PBL height for reference run conditions were significant (p?<?0.01) in ≈70% of the grid points covering Hungary. Ensemble runs using different atmospheric parameterizations and soil moisture initialization setups are also performed to analyze the sensitivity under changed conditions. In these cases, the sensitivity test showed that irrespective of the radiation and PBL scheme, the effect of different soil datasets on PBL height is roughly the same. PBL height is also sensitive to field capacity (Θf) and wilting point (Θw) changes. Θf changes seem to be more important for loamy sand, while Θw changes for the clay soil textural class. 相似文献
88.
Carla Roncoli Norman Breuer David Zierden Clyde Fraisse Kenneth Broad Gerrit Hoogenboom 《Climatic change》2012,113(3-4):1113-1121
This article illustrates how a wildfire risk forecast evolved iteratively based on stakeholder consultations. An assessment based on phone interviews indicates that such forecasts can assist fire management decisions, such as deployment of human, financial, and material resources and management of forest, timber, and habitats, and public safety. But careful attention to communication, collaboration, and capacity building is key to realizing this potential. 相似文献
89.
Alexandra Lutz James M. Thomas Greg Pohll Mamadou Keita W. Alan McKay 《Environmental Geology》2009,58(7):1441-1450
The following paper describes the goals and some preliminary work in the Bani sustainability study, an ongoing project in
Mali, West Africa. Rural communities in Mali are increasingly relying on hand-pumps, which tap groundwater resources, as a
means of obtaining potable water. The long-term sustainable yield of groundwater resources is not known but can be evaluated
in sustainability study. In 2005, a groundwater sustainability study was established along the Bani River of Mali. The Bani
study collected groundwater levels that were used in a conceptual groundwater flow model—the Bani model—to develop an understanding
of current aquifer conditions and to make limited predictions of sustainability under various future scenarios. The Bani model
showed the climatic parameters of recharge (derived from precipitation) and evapotranspiration to influence simulated groundwater
levels and groundwater volume available, while increased pumping rates, due to population growth, showed little effect. When
considered in the context of the actual Bani sustainability study area, the change in groundwater levels resulting from climatic
parameters may have negative implications, especially during several consecutive years of decreased precipitation, such as
drought, or if downward trends anticipated for precipitation continue. 相似文献
90.
The spatial distribution of polyfluoroalkyl compounds (PFCs) was investigated in dab (Limanda limanda) bile fluids collected from Iceland and the North Sea. Concentrations of various PFCs, including perfluorinated sulfonates (C4-C6, C8 PFSAs), perfluorinated carboxylic acids (C9-C14 PFCAs) and n-methyl perfluorooctane sulfonamidoethanol (MeFOSE), were quantified. Perfluorooctane sulfonate (PFOS) was the predominant compound with highest concentrations along the Danish and German coast (mean 9.36 ng/g wet weight (ww)). Significantly lower PFOS concentrations were found at the other sampling stations in the North Sea and Iceland (p < 0.01, t-test). Conversely, the spatial distribution of the PFCAs in Iceland and the North Sea was more uniform. The most abundant PFCA was perfluorononanoic acid (PFNA), while the mean concentration decreased with increasing chain length from 4.7 ng/g ww for PFNA to 0.04 ng/g ww for perfluorotetradecanoic acid (PFTeDA). Overall, the different spatial distribution of PFCs indicates different origin of sources and different transportation mechanism. 相似文献