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41.
H. JOHN B. BIRKS HEIKKI SEPPÄ 《Boreas: An International Journal of Quaternary Research》2010,39(4):655-673
Birks, H. J. B. & Seppä, H. 2010: Late‐Quaternary palaeoclimatic research in Fennoscandia – A historical review. Boreas, Vol. 39, pp. 655–673. 10.1111/j.1502‐3885.2010.00160.x. ISSN 0300‐9483. Ideas and understanding of Late‐Quaternary climatic history, especially in the Lateglacial and the postglacial, were initiated in Fennoscandia in the 19th century with pioneering studies on peat stratigraphy, megafossils and macrofossils. This review traces the history of palaeoclimatic research and the development of current ideas about climatic changes, with particular reference to the Lateglacial and its rapid climatic fluctuations, such as the Younger Dryas period, and to the Holocene, with its thermal maximum and shifts in precipitation. 相似文献
42.
Abstract There are considerable difficulties in assembling global hydrological data sets in near real time, data that might be used for deciding investment for sustainable water resources development and management, for environmental protection and for studying global change. Several reasons exist for these difficulties, a new one is that many countries have recently been cutting back on hydrological networks and the services that operate them. This means that knowledge of the World's water resources is getting worse when the global demand for water is accelerating. By way of contrast, meteorologists have ready access to large volumes of global data, much of it in real time, principally through WMO's World Weather Watch (WWW). A World Hydrological Cycle Observing System (WHYCOS) is proposed to facilitate access to global data and support hydrological services in need. A world-wide network of about 1000 stations is planned for the largest rivers, together with associated data bases and products to meet the needs of users. WHYCOS would start in Africa with a 100-station network and be expanded to other regions. It is a necessary tool for averting the coming water crisis and essential to the drive towards sustainable development. 相似文献
43.
New data, derived from microprobe analyses of melting experiments,are presented in the form of sub-projections in the model basaltsystem, Ol-Pl-Wo-SiO2, to illustrate the shifts in the liquidusfields of olivine, plagioclase, spinel, pyroxene, and silicain low-alkali liquids as functions of variable Wo componentand Mg. The projections are calculated in terms of oxygen unitsto avoid the non conservative properties of moleunits and to provide a better representation of the volume proportionsof minerals. These projections show that over a wide range ofcomposition the complex, natural basalt system has liquidusboundaries that resemble many of those in the simpler CaO-MgO-Al2O3-SiO2system. One important feature of the natural system is the progressivechange in the dominant low-Ca pyroxene along the olivine liquidussurface from protoenstatite to orthoenstatite to pigeonite asMg decreases. Another notable feature is the expansion of theplagioclase liquid field at the expense of the olivine and low-Capyroxene fields as Mg decreases in low-alkali liquids. Increasingalkali concentration has almost exactly the opposite effectso that evolved terrestrial basalts have higher proportionsof feldspar components than their lunar and eucritic counterparts. The new phase diagrams indicate that low-alkali liquids residualto those that produced the ancient, ferroan lunar anorthositesshould have crystallized an amount of ferro-quartz-gabbro equivalentto 10 per cent of the volumes of their parents. The scarcityof such rocks among the returned lunar samples poses a problemfor simple models of lunar petrogenesis. 相似文献
44.
Dolomitized intervals of a core from San Salvador Island, Bahamas, exhibit variations of two texturally and geochemically distinct end-members. In the Pliocene section of the dolomitized interval, the two end-members alternate in a pattern that may reflect originally and/or diagenetically modified depositional facies. Formerly mud-free intervals, locally capped by exposure surfaces are massive crystalline, mimetic dolomites (CM). Muddier sediments are replaced by friable microsucrosic dolomites (MS). CM and MS dolomites also differ in porosity (< 10% vs > 30%), permeability (< 10 md vs > 100 md), mol% MgCO3 (44–9 vs 47–7) mol%), oxygen isotopic composition (1–7 vs 2–7‰) and strontium content (241 vs 106 ppm). These data indicate that depositional and diagenetic fabric are the principal controls governing the distribution of dolomite types. Differences in texture and geochemistry are suggested as arising through differential rates of crystallization produced as a result of variations in permeability and reactivity of the precursor sediments and rocks. 相似文献
45.
Imbricate wedge marks (facets) on garnets in sandstones of the Cambrian Munising Formation of northern Michigan are associated with mouldic secondary porosity developed at the expense of garnet. Mouldic pores surrounding faceted garnets indicate that garnets in these sandstones have been affected by intrastratal dissolution (retreat of the mineral surface from its original boundaries) rather than by grain enlargement, which would be expected if garnet overgrowths had formed. The association of garnet facets with textural evidence of garnet dissolution proves that garnet facets form by intrastratal dissolution. These results confirm similar findings in other recent studies, and extend the geographic and stratigraphic range of proven occurrences of facet formation by intrastratal dissolution. 相似文献
46.
The Scots Bay formation, Nova Scotia, Canada, a Jurassic carbonate lake with Silica-rich hydrothermal springs 总被引:1,自引:0,他引:1
During Early Jurassic time, the Scots Bay Formation accumulated in an aerobic lake on the floor of the subtropical Fundy rift valley. A diverse biota flourished in the lake as evidenced by algal stromatolites, oncolites, charophytes, ostracods, gastropods, conchostracans, fish bones, calcispheres and logs. Carbonate wackestone and packstone were deposited in the littoral zone and lime mudstone accumulated offshore on a proximal slope. Silica-rich hydrothermal springs and seeps around and on the floor of the lake precipitated siliceous tufa and silicified adjacent carbonate strata. The tufa is characterized by the progressive sequence: (1) open-framework, porous substrate of goethite spheres, (2) encrusting chalcedony spherulites where goethite inclusions decrease in size and number outwards towards the surfaces of the spherulites, (3) a fringe of quartz on the chalcedony spherulites and (4) coarsening inwards mosaics of quartz that filled the remaining voids. Carbonate diagenesis included conversion of low-Mg calcite ooze to micrite and microspar-pseudospar, and local dissolution and reprecipitation of calcite cement. At times the lake shrank in size, concentrating silica in increasingly alkaline lake water which then silicified some of the carbonate strata and logs. The latest cements were calcite, zeolites and celadonite. 相似文献
47.
The Geochemistry and Experimental Petrology of Sodic Alkaline Basalts from Oatlands, Tasmania 总被引:2,自引:2,他引:2
Sodic basalts of Oligocene-Early Micene age occur within anEarly Tertiary graben in the Oatlands district of Tasmania.They include olivine tholeiites, alkali olivine basalts, basanites,transitional nephelinites, nepheline hawaiites, and nephelinemugearites. They have compositional characteristics in commonwith sodic alkaline basalt suites from other parts of the world.With decreasing SiO2, concentrations of CaO, alkalis, P2O5,and incompatible trace elements increase. Compositional and experimental data for the basalts are consistentwith their derivation by polybaric partial melting of a garnetlherzolite source enriched in P2O5, light rare earths, Nb, andother incompatible trace elements. Experimental data for a primitivenepheline basanite from the Oatlands district indicate thatconcentrations of H2O+CO2 need not have been more than 6?5 wt.%for the original basanite magma to have derived from an amphibole-bearinggarnet lherzolite source. In the case of more SiO2-undersaturatedolivine melilitites from the neighbouring Central Plateau, theexperimental evidence is consistent with either higher concentrationsof H2O+CO2 (approaching 14 wt.%), or higher pressures of origin(>35 kb). Petrographic and geochemical evidence suggeststhat the latter is the more probable of the alternatives. 相似文献
48.
Gypsum and anhydrite fabrics observed in trenches and deep (500 m) cores from Bristol Dry Lake, California, USA, exhibit a vertical alignment of crystals similar to the fabric seen in bottom-nucleated brine pond gypsum. However, geochemical and sedimentological evidence indicate that the gypsum formed in Bristol Dry Lake precipitated displacively within the sediment where groundwater saturated with respect to gypsum recharges around the playa margin (groundwater-seepage gypsum). Evidence for displacive growth of gypsum is: (i) the geometry of the deposit, (ii) stable isotopic data and the water chemistry of the brine, and (iii) inclusions of matrix which follow twin planes and completely surround crystals as they grow. The bulk of the gypsum precipitated in the playa occurs around the edges of the playa in the playamargin facies and completely rings the lake. Sulphate concentrations in the groundwater increase toward the gypsum zone in the playa margin. Basinward of this zone, sulphate concentrations decrease sharply to trace element levels in the basin centre brine. Authigenic gypsum is rare in the centre of the playa. Stable (δ18O values measured for gypsum waters of crystallization (GWC) are similar to the values calculated for groundwater in the playa margin and alluvial fan sediments (?– 6%0), whereas measured brine δ18O values range from + 0·5 to + 3·7%0. Deuterium values measured for groundwater are ?– 70%0, GWC are ?– 60 to – 65%0 and brine values are ?– 57%0. The geometry of the deposit and the chemical data suggest that the water precipitating the gypsum is more closely associated with the groundwater than the brine. However, some mixing between groundwater and brine is likely. Within 100 m of the surface, the gypsum dehydrates to anhydrite, although the same vertically aligned fabric is retained through the diagenetic process. The similarity of displacive vertically aligned gypsum and anhydrite fabrics seen in Bristol Dry Lake to subaqueously deposited gypsum in modern brine ponds indicates that the criteria used to define subaqueous fabrics must be better constrained. 相似文献
49.
50.
The Transition to Potassic Alkaline Volcanism in Island Arcs: The Ringgit--Beser Complex, East Java, Indonesia 总被引:4,自引:0,他引:4
EDWARDS CAROLINE M. H.; MENZIES MARTIN A.; THIRLWALL MATTHEW F.; MORRIS JULIE D.; LEEMAN WILLIAM P.; HARMON RUSS S. 《Journal of Petrology》1994,35(6):1557-1595
The origin of potassic lavas with within-plate characteristicsin island are settings is unclear. The volcanic complex of RinggitBeser,situated in eastern Java, has erupted lavas of both normal islandare calc-alkaline type and atypical potassic lavas, includingsome highly magnesian lavas. The occurrence of these primitivelavas gives an unusual insight into the source characteristicsof the potassic lavas. The lavas from RinggitBeser have a wide range of K2O(1.16.4 wt. %) and MgO contents (18.01.6 wt.%).The most magnesian lavas have high Ni and Cr contents. The calc-alkalinelavas have incompatible trace element patterns typical of islandare lavas with enrichments in large ion lithophile elements(LILE) and light rare earth elements (LREE) relative to highfield strength elements (HFSE) and heavy REE (HREE). The potassiclavas may be divided into two series on the basis of Ba andNb contents, with the enriched potassic (EK) series having higherBa and Nb contents for a given MgO content than the potassic(K) series. The EK and K series lavas have some incompatibletrace element ratios similar to within-plate lavas (e.g., highCe/Pb, low LILE/HFSE ratios, and low B/Be). However, both theEK series and K series lavas have negative Ti and Zr anomalies,and the EK series lavas have high Ba/La similar to are lavas.There is little distinction in Sr and Nd isotopes between theK and EK series, but the calc-alkaline lavas have lower 87Sr/86Srand higher 143Nd/144Nd ratios than the potassic lavas. The EKseries lavas have lower 206Pb/204Pb and higher 208Pb/204Pb thanthe K series lavas, but similar 207Pb/204Pb ratios. The K serieslavas define an almost horizontal trend in 207Pb206Pbspace. The Pb isotopic ratios indicate that the EK series lavasare derived from a single mantle source, whereas the K seriesoriginate from a mixture of two mantle components. Calc-alkalinelavas have Pb isotope ratios similar to other calc-alkalineand tholeiitic lavas from Java, and plot on a mixing line betweenIndian Ocean mid-ocean ridge basalt (MORB) and Indian Oceansediment. Incompatible trace element and Pb isotope data for the calc-alkalinelavas indicate that these lavas have a similar source to othercalc-alkaline lavas erupted in Java, namely melts of the IndianOcean MORB mantle fluxed by fluids from the subducted slab.The potassic lavas originate from enriched mantle sources withinthe wedge which have not been affected by recent subductionprocesses. The EK series lavas are derived from a metasomatizedzone which has EMI-type characteristics. The K series lavasare derived from mixing of melts from Christmas Island-type(EMII) mantle and the metasomatized zone. The metasomatizedzone is probably situated at the base of the lithosphere andthe Indian Ocean MORB and Christmas Island-type mantle componentsare situated in the asthenosphere of the wedge. Isotopic datafor RinggitBeser lavas confirm that the mantle wedgeof the Sunda arc is extremely heterogeneous (Foden & Varne,1980; Varne, 1985; Wheller et al., 1987). The similarity in geochemistry between Indonesian potassic lavasand those erupted in continental settings indicates that themagma source is essentially the same, namely a metasomatizedphlogopite-rich layer generated by melts of recycled subductedlithosphere. The lack of negative Ti anomalies in the continentalpotassic lavas is ascribed to lower oxidation states in themantle in continental settings. 相似文献