Evidence for plunging river plume deposits in the Pahrump Hills member of the Murray formation,Gale crater,Mars     

Kathryn M. Stack  John P. Grotzinger  Michael P. Lamb  Sanjeev Gupta  David M. Rubin  Linda C. Kah  Lauren A. Edgar  Deirdra M. Fey  Joel A. Hurowitz  Marie McBride  Frances Rivera‐Hernndez  Dawn Y. Sumner  Jason K. Van Beek  Rebecca M. E. Williams  Robin Aileen Yingst 《Sedimentology》2019,66(5):1768-1802

Recent robotic missions to Mars have offered new insights into the extent, diversity and habitability of the Martian sedimentary rock record. Since the Curiosity rover landed in Gale crater in August 2012, the Mars Science Laboratory Science Team has explored the origins and habitability of ancient fluvial, deltaic, lacustrine and aeolian deposits preserved within the crater. This study describes the sedimentology of a ca 13 m thick succession named the Pahrump Hills member of the Murray formation, the first thick fine‐grained deposit discovered in situ on Mars. This work evaluates the depositional processes responsible for its formation and reconstructs its palaeoenvironmental setting. The Pahrump Hills succession can be sub‐divided into four distinct sedimentary facies: (i) thinly laminated mudstone; (ii) low‐angle cross‐stratified mudstone; (iii) cross‐stratified sandstone; and (iv) thickly laminated mudstone–sandstone. The very fine grain size of the mudstone facies and abundant millimetre‐scale and sub‐millimetre‐scale laminations exhibiting quasi‐uniform thickness throughout the Pahrump Hills succession are most consistent with lacustrine deposition. Low‐angle geometric discordances in the mudstone facies are interpreted as ‘scour and drape’ structures and suggest the action of currents, such as those associated with hyperpycnal river‐generated plumes plunging into a lake. Observation of an overall upward coarsening in grain size and thickening of laminae throughout the Pahrump Hills succession is consistent with deposition from basinward progradation of a fluvial‐deltaic system derived from the northern crater rim into the Gale crater lake. Palaeohydraulic modelling constrains the salinity of the ancient lake in Gale crater: assuming river sediment concentrations typical of floods on Earth, plunging river plumes and sedimentary structures like those observed at Pahrump Hills would have required lake densities near freshwater to form. The depositional model for the Pahrump Hills member presented here implies the presence of an ancient sustained, habitable freshwater lake in Gale crater for at least ca 10³ to 10⁷ Earth years.  相似文献   

Hydro-Climatic Trends of the Yellow River Basin for the Last 50 Years   总被引：10，自引：0，他引：10  

Guobin Fu  Shulin Chen  Changming Liu  Dawn Shepard 《Climatic change》2004,65(1-2):149-178

Kendall's test was used to analyze the hydro-climatic trends of the Yellow River over the last half century. The results show that: (1) the runoff of the basin has decreased even after allowing for human uses, (2) the watershed has become warmer with a more significant increase in minimum temperature than in mean and maximum temperatures, and (3) no significant change in precipitation trend was observed. The major reasons for these results include human activities, global warming, land use/land cover change, and others, such as accuracy of natural runoff estimation, precipitation characteristics, groundwater exploitation, water transfer, and snowmelt. Homogeneity analysis indicated that precipitation, temperature, maximum temperature, and minimum temperature were all heterogeneous and the trends varied from region to region and from month to month. If the Intergovernmental Panel on Climate Change (IPCC) projections of continued warming in the region during the 21st century are correct, the present results then suggest that the trend towards reduced runoff is likely to lead to exacerbated problems for agriculture, industry, urban communities, and the overall regional environment.  相似文献   

Consolidation-related fabric changes of periplatform sediments     

Richard Rezak  Dawn L. Lavoie 《Geo-Marine Letters》1990,10(2):101-109

Geotechnical properties of carbonate sediments result from several factors such as the particular constituents comprising the sediment, the mineralogy, fabric, and effective stress. Investigating the effects of increasing effective stress by mechanical consolidation using permeability, porosity, and porometry determinations reveals fabric changes that could not be determined in scanning electron micrographs. Porometry changes, determined using an image analyzer, are a function of matrix composition and grain support. Samples that were predominantly matrix-supported exhibited an increase in pore numbers per unit area and a pore size decrease resulting from consolidation. Samples composed predominantly of aragonite needle matrices displayed opposite behavior.  相似文献   

Sulfur dioxide emissions and degassing behavior of Erebus volcano,Antarctica     

Dawn Sweeney  Philip R. Kyle  Clive Oppenheimer 《Journal of Volcanology and Geothermal Research》2008

Emission rates of sulfur dioxide (SO₂) were measured at Erebus volcano, Antarctica in December between 1992 and 2005. Since 1992 SO₂ emissions rates are normally distributed with a mean of 61 ± 27 Mg d^− 1 (0.7 ± 0.3 kg s^− 1) (n = 8064). The emission rates vary over minutes, hours, days and years. Hourly and daily variations often show systematic and cyclic trends. Long-wavelength, large amplitude trends appear related to lava lake area and both are likely controlled by processes occurring at depth. Time series analysis of continuous sequences of measurements obtained over periods of several hours reveals periodicity in SO₂ output ranging from 10 to 360 min, with a 10 min cycle being the most dominant. Closed and open-system degassing models are considered to explain observed variable degassing rates. Closed-system degassing is possible as rheological stiffening and stick/slip may occur within the system. However, the timescales represented in these models do not fit observations made on Erebus. Open-system degassing and convection fits the observations collected as the presented models were developed for a system similar to Erebus in terms of degassing, eruptive activity and process repose time. We show that with the observed emission rate (0.71 kg s^− 1) and a crystal content of 30%, magma will cool 65 °C to match observed heat fluxes; this cooling is sufficient enough to drive convection.  相似文献   

Modeling Coronal Loop Abundances: Effects of Parameter Variations on Observables     

Lenz  Dawn D. 《Solar physics》2000,193(1-2):131-137

Coronal abundance variations arise from and affect solar atmospheric processes such as coronal heating and structural dynamics. Lenz (1999) presented initial results of a numerical theoretical study of abundances and ion heating rates in static, steady-state coronal loops. We present here a closer investigation of two fundamental aspects of the physics of coronal abundances, relating modeling parameters to observables: (1) the effect of varying the abundances on the electron temperature and (2) the effect of varying the ion heating rate on abundances.  相似文献   

Tectonometamorphic evolution of the tip of the Himalayan metamorphic core in the Jajarkot klippe,west Nepal     

Renaud Soucy La Roche  Laurent Godin  John M. Cottle  Dawn A. Kellett 《Journal of Metamorphic Geology》2019,37(2):239-269

New phase equilibrium modelling, combined with U–Th/Pb petrochronology on monazite and xenotime, and ⁴⁰Ar/³⁹Ar geochronology on white mica, reveal the style of deformation and metamorphism near the southern tip of the extruded Himalayan metamorphic core (HMC). In the Jajarkot klippe, west Nepal foreland, greenschist to lower amphibolite facies metamorphism is entirely constrained to the Cenozoic Himalayan orogeny, in contrast with findings from other foreland klippen in the central Himalaya. HMC rocks exposed in the Jajarkot klippe yield short‐lived, hairpin pressure–temperature–time–deformation paths that peaked at 550–600°C and 750–1,200 MPa at 25 Ma. The Main Central thrust (MCT) and the South Tibetan detachment (STD) bound the base and the top of the HMC, respectively, and were active simultaneously for at least part of their deformation history. The STD was active at c. 27–26 Ma and possibly as late as c. 19 Ma, while the MCT may have been active as early as 27 Ma and was still active at c. 22 Ma. The tectonometamorphic conditions in the Jajarkot klippe are characteristic of crustal thickening and footwall accretion of new material at the tip of the extruding metamorphic orogenic core. Our new results reveal that collisional processes active in the middle to late Miocene at the base of the HMC now exposed in the hinterland were also active earlier, during the Oligocene, at the tip of the southward‐extruding middle crust.  相似文献   

Genomics in marine monitoring: New opportunities for assessing marine health status     

Sarah J. Bourlat  Angel Borja  Jack Gilbert  Martin I. Taylor  Neil Davies  Stephen B. Weisberg  John F. Griffith  Teresa Lettieri  Dawn Field  John Benzie  Frank Oliver Glöckner  Naiara Rodríguez-Ezpeleta  Daniel P. Faith  Tim P. Bean  Matthias Obst 《Marine pollution bulletin》2013

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Comparison of Shake and Column Silica Gel Cleanup Methods for Groundwater Extracts to Be Analyzed for TPHd/DRO     

Dawn A. Zemo  Karen A. Synowiec  Renae I. Magaw  Rachel E. Mohler 《Ground Water Monitoring & Remediation》2013,33(4):108-112

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Digital Data-Centric Geography: Implications for Geography's Frontier     

Forrest J. Bowlick  Dawn J. Wright 《The Professional geographer》2013,65(4):687-694

The debate regarding geographic information systems (GIS) as tool, toolbox, or science still lingers in geography departments and among geographers. Analysis of geographic information is a vital component of decision making among business, governments, researchers, and academics. GIS users, geographers and nongeographers alike, use and benefit from problem-solving methods in numerous fields and contexts, making the use of GIS and the core competencies associated with using GIS a topic of intense debate. Complicating this ongoing discussion is the rise of data-centric approaches to research in geography that further expand the capabilities of spatial analysis and add to the expected knowledge of a GIS user and analyst. Building on a panel discussion at the 2016 American Association of Geographers (AAG) annual meeting, as well as informal dialogues on Twitter and other social media platforms that navigate this issue in academics and industry, this article explores how skills in research computing and programming operate in geography and GIS, especially given the rise of data-centric approaches to research in these realms. Some topics, like the costs and benefits of open and closed source software, are familiar from previous discussions in geography and GIS. Others, though, like the reward structures and recognition for computing skills or programming ability, have not been widely considered given the current landscape.  相似文献   

Soundings: The Story of the Remarkable Woman Who Mapped the Ocean Floor. By Hali Felt     

Dawn J. Wright 《Geographical review》2014,104(1):115-117

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