The scattered trans-Neptunian object 1998 XY95     

S.J. Collander-Brown  A. Fitzsimmons  E. Fletcher  M.J. Irwin  I.P. Williams 《Monthly notices of the Royal Astronomical Society》2001,325(3):972-978

On 1998 December 12 a new trans-Neptunian object, 1998 XY95, was discovered as part of a deep search. Recent observations of this object have placed it amongst the class of objects known as the scattered trans-Neptunian objects (TNOs). A total of 39 CCD images of 1998 XY95 were taken over two nights, and these were used to search for a light curve, but no significant periodicity was found. An examination of the possible orbital evolution gives no indication of how it may have arrived on its present orbit. The current best-fitting orbit is unstable, but remains within a band of semi-major axis approximately 2 au wide. The bottom of this band is due to 3:1 mean motion resonance with Neptune, while the reason for the top of the band remains unclear.  相似文献   

Potassium chlorate—hydrochloric acid: a sulphide selective leach for bedrock geochemistry     

M. Olade  K. Fletcher 《Journal of Geochemical Exploration》1974,3(4):337-344

Potassium chlorate—hydrochloric acid is compared to ascorbic acid—hydrogen peroxide, aqua regia, and nitric—perchloric as a sulphide-selective leach for bedrock geochemistry. Results obtained on granodiorite samples containing copper sulphides indicate that the procedure is probably more selective than the other leaches and has the advantages of rapidity and simplicity.  相似文献   

OSS (Outer Solar System): a fundamental and planetary physics mission to Neptune, Triton and the Kuiper Belt     

B. Christophe  L. J. Spilker  J. D. Anderson  N. André  S. W. Asmar  J. Aurnou  D. Banfield  A. Barucci  O. Bertolami  R. Bingham  P. Brown  B. Cecconi  J. -M. Courty  H. Dittus  L. N. Fletcher  B. Foulon  F. Francisco  P. J. S. Gil  K. H. Glassmeier  W. Grundy  C. Hansen  J. Helbert  R. Helled  H. Hussmann  B. Lamine  C. L?mmerzahl  L. Lamy  R. Lehoucq  B. Lenoir  A. Levy  G. Orton  J. Páramos  J. Poncy  F. Postberg  S. V. Progrebenko  K. R. Reh  S. Reynaud  C. Robert  E. Samain  J. Saur  K. M. Sayanagi  N. Schmitz  H. Selig  F. Sohl  T. R. Spilker  R. Srama  K. Stephan  P. Touboul  P. Wolf 《Experimental Astronomy》2012,34(2):203-242

  相似文献   

Identifying saltcedar with hyperspectral data and support vectormachines     

Reginald S. Fletcher  James H. Everitt  Chenghai Yang 《国际地球制图》2013,28(3):195-209

Saltcedar (Tamarix spp.) are a group of dense phreatophytic shrubs and trees that are invasive to riparian areas throughout the United States. This study determined the feasibility of using hyperspectral data and a support vector machine (SVM) classifier to discriminate saltcedar from other cover types in west Texas. Spectral measurements were collected with a ground-based hyperspectral spectroradiometer (spectral range 350–2500 nm) in December 2008 and April 2009. Spectral data consisting of 1698 spectral bands (400–1349, 1441–1789, 1991–2359 nm) were subjected to a support vector machine classification to differentiate saltcedar from other vegetative and non-vegetative classes. For both dates, a linear kernel model with a C value (error penalty) of 100 was found optimum for separating saltcedar from the other classes. It identified saltcedar with accuracies ranging from 95% to 100%. Findings support further exploration of hyperspectral remote sensing technology and SVM classifiers for differentiating saltcedar from other cover types.  相似文献   

Deposition of 1.88-billion-year-old Iron Formations as a Consequence of Rapid Crustal Growth     

Birger Rasmussen  Ian R. Fletcher  Andrey Bekker  Janet R. Muhling  Courtney J. Gregory  Alan M. Thorne 《Journal of the Geological Society of India》2012,80(1):147

  相似文献   

Zirconolite and xenotime U–Pb age constraints on the emplacement of the Golden Mile Dolerite sill and gold mineralization at the Mt Charlotte mine,Eastern Goldfields Province,Yilgarn Craton,Western Australia     

Birger Rasmussen  Andreas G. Mueller  Ian R. Fletcher 《Contributions to Mineralogy and Petrology》2009,157(5):559-572

In situ SHRIMP U–Pb dating of magmatic zirconolite (CaZrTi₂O₇) in the Golden Mile Dolerite from the Mt Charlotte gold deposit (Yilgarn Craton, Australia) has yielded the first robust emplacement age (2,680 ± 9 Ma) for the principle host-rock of gold mineralization in the Kalgoorlie district. In contrast, co-magmatic zircon gave ages from ~2.68 Ga to ~2.17 Ga, reflecting isotopic resetting of high-U and -Th crystals. In situ SHRIMP analysis of hydrothermal xenotime (YPO₄), which co-exists with gold in alteration pyrite, provided a Pb/Pb isochron age of 2,655 ± 13 Ma. This date indicates that the youngest deposit in the Kalgoorlie district (Mt Charlotte) formed at ~2.65 Ga, and provides a new minimum age for the structurally older Golden Mile deposit. Our results indicate that gold mineralization at Mt Charlotte is ~50 million years older than indicated by recent ⁴⁰Ar/³⁹Ar dating and places new constraints on the timing of late-stage regional faulting (D₄) in the province.  相似文献   

Understanding fracture distribution and its relation to knickpoint evolution in the Rio Icacos watershed (Luquillo Critical Zone Observatory,Puerto Rico) using landscape-scale hydrogeophysics     

Xavier Comas  William Wright  Scott A. Hynek  Raymond C. Fletcher  Susan L. Brantley 《地球表面变化过程与地形》2019,44(4):877-885

The Rio Icacos watershed in the Luquillo Mountains (Puerto Rico) is unique due to its extremely rapid weathering rates. The watershed is incised into a quartz diorite that has developed a large knickzone defining the river profile. Regolith thickness within the watershed generally decreases from 20 to 30 m at the ridges to several meters in the quartz diorite-dominated valley to tens of centimeters near the major river knickpoint, as determined from previous studies. Above the knickzone, we observe spheroidal corestones, but below this weathering is much less apparent. Measured erosion rates from previous studies are also high in the knickzone compared with upper elevations within the river profile. A suite of near-surface geophysical methods (i.e. ground penetrating radar and terrain conductivity) capable of fast data acquisition in rugged landscapes, was deployed at kilometer scales to characterize critical zone structure. Concentrations of chaotic ground penetrating radar (GPR) reflections and diffraction hyperbolas with low electrical conductivity were observed in vertical zones that outcrop at the land surface as areas of intense fracturing and spheroidally weathered corestones. The width of these fractured and weathered zones showed an increase with proximity to the knickpoint, and was attributed to dilation of these sub-vertical fractures near the knickpoint, as postulated theoretically by a stress model calculated for the topographic variability across the knickzone in the Rio Icacos, and that shows a release of compressive stress near the knickpoint. We hypothesize that erosion rates increase in the knickzone because of this inferred dilation of fractures. Specifically, opened fractures could enhance access of water and in turn promote spalling, erosion, and spheroidal weathering. This study shows that ground-based hydrogeophysical methods used at the landscape-scale (traditionally applied at smaller scales) can be used to explore critical zone architecture at the scales needed to explain the extreme variability in erosion rates across river profiles. © 2018 John Wiley & Sons, Ltd.  相似文献   

A comparison of pollen extraction methods confirms dense‐media separation as a reliable method of pollen preparation          下载免费PDF全文

J. F. E. Campbell  W. J. Fletcher  P. D. Hughes  E. L. Shuttleworth 《第四纪科学杂志》2016,31(6):631-640

  相似文献   

Radiogenic heating and craton‐margin plate stresses as drivers for intraplate orogeny          下载免费PDF全文

F. J. Korhonen  S. P. Johnson  M. T. D. Wingate  C. L. Kirkland  I. R. Fletcher  D. J. Dunkley  M. P. Roberts  S. Sheppard  J. R. Muhling  B. Rasmussen 《Journal of Metamorphic Geology》2017,35(6):631-661

The Proterozoic belts that occur along the margins of the West Australian Craton, as well as those in intraplate settings, generally share similar geological histories that suggest a common plate‐margin driver for orogeny. However, the thermal drivers for intraplate orogenesis are more poorly understood. The Mutherbukin Tectonic Event records a protracted period of Mesoproterozoic reworking of the Capricorn Orogen and offers significant insight into both the tectonic drivers and heat sources of long‐lived intraplate orogens. Mineral assemblages and tectonic fabrics related to this event occur within a 50 km‐wide fault‐bound corridor in the central part of the Gascoyne Province in Western Australia. This zone preserves a crustal profile, with greenschist facies rocks in the north grading to upper amphibolite facies rocks in the south. The P–T–t evolution of 13 samples from 10 localities across the Mutherbukin Zone is investigated using phase equilibria modelling integrated with in situ U–Pb monazite and zircon geochronology. Garnet chemistry from selected samples is used to further refine the P–T history and shows that the dominant events recorded in this zone are prolonged D₁ transpression between c. 1,320 and 1,270 Ma, followed by D₂ transtension from c. 1,210 to 1,170 Ma. Peak metamorphic conditions in the mid‐crust reached >650°C and 4.4–7 kbar at c. 1,210–1,200 Ma. Most samples record a single clockwise P–T evolution during this event, although some samples might have experienced multiple perturbations. The heat source for metamorphism was primarily conductive heating of radiogenic mid‐ and upper crust, derived from earlier crustal differentiation events. This crust was thickened during D₁ transpression, although the thermal effects persisted longer than the deformation event. Peak metamorphism was terminated by D₂ transtension at c. 1,210 Ma, with subsequent cooling driven by thinning of the radiogenic crust. The coincidence of a sedimentary basin acting as a thermal lid and a highly radiogenic mid‐crustal batholith restricted to the Mutherbukin Zone accounts for reworking being confined to a discrete crustal corridor. Our results show that radiogenic regions in the shallow to mid crust can elevate the thermal gradient and localize deformation, causing the crust to be more responsive to far‐field stresses. The Mutherbukin Tectonic Event in the Capricorn Orogen was synchronous with numerous Mesoproterozoic events around the West Australian Craton, suggesting that thick cratonic roots play an important role in propagating stresses generated at distant plate boundaries.  相似文献   

Release and transformations of inorganic iodine by marine macroalgae     

Rosie Chance  Alex R. Baker  Frithjof C. Küpper  Claire Hughes  Bernard Kloareg  Gill Malin 《Estuarine, Coastal and Shelf Science》2009

A number of field and laboratory studies on the impact of marine macroalgae on dissolved inorganic iodine speciation are presented. Within tidally isolated rock pools, the brown macroalga Fucus serratus was found to both release stored iodide and to facilitate the reduction of iodate to iodide. In contrast, no discernible changes in iodine speciation were observed in rock pools containing green macroalgae of the genus Ulva. Incubation experiments confirmed that the macroalgae Laminaria digitata, F. serratus and Kallymenia antarctica release iodide, though the rate of release varied between species and between specimens of the same species. Application of oxidative stress by treatment with cell wall derived oligoguluronate elicitors increased the efflux of iodide by L. digitata approximately 20-fold. The release of iodide by macroalgae may impact upon the formation of volatile iodine species (molecular iodine and iodocarbons) that are of importance in the coastal atmosphere.  相似文献