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141.
A. H. F. Robertson O. Parlak N. Yıldırım P. Dumitrica K. Taslı 《International Journal of Earth Sciences》2016,105(1):167-201
Evidence of rifting and continental break-up to form the S Neotethys is found within the volcanic-sedimentary Koçali Complex. This is a folded, thrust-imbricated succession that includes lavas, volcaniclastic sediments, pelagic carbonates, radiolarites and manganiferous deposits. Interbedded ribbon cherts contain radiolarians of Late Triassic to Late Jurassic age. The lower part of the succession of Mid?-Late Triassic age (Tarasa Formation) is dominated by enriched mid-ocean ridge basalt (E-MORB). The overlying Late Triassic to Mid-Jurassic interval (Konak Formation) is characterised by intercalations of ocean island basalt and E-MORB. Taking account of structural position, the basalts erupted within the outer part of a continent–ocean transition zone. Continental break-up probably occurred during the Late Triassic (Carnian–Norian). Early to Mid-Jurassic lavas and volcaniclastic sediments record volcanism probably after continental break-up. In addition, the Karadut Complex is a broken formation that is located at a relatively low structural position just above the Arabian foreland. Pelagic carbonates, redeposited carbonates and radiolarites predominate. Radiolarians are dated as Early to Mid-Jurassic and Late Cretaceous in age. The pelagic carbonates include planktic foraminifera of Late Cretaceous age. The Karadut Complex resulted from the accumulation of calcareous gravity flows, pelagic carbonate and radiolarites in a relatively proximal, base-of-slope setting. After continental break-up, MORB and ophiolitic rocks formed within the S Neotethys further north. Tectonic emplacement onto the Arabian platform took place by earliest Maastrichtian time. Regional interpretation is facilitated by comparisons with examples of Triassic rifting and continental break-up in the eastern Mediterranean region and elsewhere. 相似文献
142.
Dr. Ing. Antal Ádám Dipl. Geophys. András Erkel Lászlò Szabadváry 《Pure and Applied Geophysics》1962,52(1):127-138
Zusammenfassung Die Einleitung gibt einige Gesichtspunkte der heutigen geoelektrischen Instrumentenentwicklung in Ungarn. Dann werden zwei neue ungarische geoelektrische Instrumente u.z.w.: 1) ein den spezifischen Widerstand unmittelbar lieferndes Instrument und 2) ein isolationsfehlerloses geophysikalisches Fotoregistrier-instrument mit ihren theoretischen Grundlagen behandelt. Am Ende des Artikels werden einige technische Daten der Instrumenten mitgeteilt.
Summary The introduction deals with the general aspects of the development of modern geoelectrical instruments in Hungary. Then two hungarian geoelectrical instruments: 1) an instrument giving directly the value of the resistivity and 2) a geophysical recording instrument free from isolation errors are discussed from the point of view of the theoretical problems of the instrument-constructions. Finally some technical data of the instruments are presented.相似文献
143.
144.
The saturation of calcite and aragonite in the Arctic Ocean 总被引:1,自引:0,他引:1
We report on the chemical saturation of CaCO3 in the waters of the Arctic Ocean calculated from total alkalinity (AT) and total dissolved inorganic carbon (CT). Data based on four different expeditions are presented: International Arctic Ocean Expedition (IAOE-91), Arctic Ocean Section 94 (AOS94), Polarstern Arctic '96 expedition (ACSYS 96), and Joint Ocean Ice Study 97 (JOIS 97). The results show a lysocline at around 3500 m for aragonite and that most of the Arctic Ocean sea floor lies above the lysocline for calcite. The only anomaly is the low degree of saturation at the shelf break depth in the Canadian Basin seen in the sections of the AOS94 and JOIS 97 cruises, correlated with nutrient maxima and very low O2 concentration, suggesting decomposition of organic matter. The insignificant variability in degree of saturation between the deep waters of the different basins in the Arctic Ocean indicates a very low sedimentation/remineralisation of organic soft matter. 相似文献
145.
Christoffer Bostrm Emma L. Jackson Charles A. Simenstad 《Estuarine, Coastal and Shelf Science》2006,68(3-4):383
Seagrasses comprise some of the most heterogeneous landscape structures of shallow-water estuarine/marine ecosystems in the world. However, while knowledge at the molecular, organism, patch and community scale is pervasive, understanding of seagrass landscape ecology is more fragmentary and has not been synthesized. The growth and recruitment dynamics of seagrasses as well as man-made and/or natural disturbances create complex spatial configurations of seagrass over broad (metres to kilometres) spatial scales. Hence, it is important to identify mechanisms maintaining and/or threatening the diversity-promoting function of seagrass meadows and to understand their effects on benthic populations and communities. Although landscape ecology has recently become more integrated into seagrass research, our understanding of animal responses to variability in seagrass landscape structure is still fragmentary. By reviewing the literature to date, this paper evaluates studies on seagrass landscape ecology, testing the general null hypothesis that concepts developed in terrestrial settings can be generalized across landscapes, and (a) presenting definitions and terms used in seagrass landscape ecology, (b) reviewing geographical patterns of seagrass landscape studies to identify possible key regions and target species, (c) evaluating different methodological approaches, (d) describing the spatial and temporal scales used to describe organism responses to seagrass landscape structure, and (e) placing seagrass landscapes into an applied context. 相似文献
146.
Bertil
strm 《Marine Chemistry》1973,1(4):323-327
A new technique for adding Winkler reagents to water samples at sea has been developed. Expendable ampoules containing the reagents replace syringes or pipettes. The main features of the ampoules are simpler handling and safer sampling with preserved accuracy. 相似文献
147.
Ann-Sofi Smedman Knut Lundin Hans Bergström Ulf Högström 《Boundary-Layer Meteorology》1991,56(3):295-307
A highly mobile system for accurate measurements of wind speed and horizontal turbulence in the lowest few hundred meters of the atmosphere is presented. It consists of a light-weight sonde (only 50 g, including batteries that permit 12 h of continuous operation) which can be easily lifted by a small kite in winds below 5 m/s and up to at least 25 m/s. In winds below 5 m/s, a small kytoon may be used instead. The signals from the sonde are received by a standard FM-radio equipped with a frequency converter, and data are recorded on ordinary cassette tapes. Field tests against towermounted precision instruments were performed at two sites during neutral and unstable conditions with the sonde suspended 25 m below a small kite, the measuring heights being 11 and 18 m respectively during the two test series. Mean wind speeds are found to be accurate to within ±0.2 m/s. Wind speed spectra obtained with the mg src="/content/k58r5k851812j6t3/xxlarge8216.gif" alt="lsquo" align="BASELINE" BORDER="0">flyingmg src="/content/k58r5k851812j6t3/xxlarge8217.gif" alt="rsquo" align="BASELINE" BORDER="0"> sonde can be evaluated up to 0.5 Hz and are found to agree closely with the spectra of the longitudinal component recorded simultaneously by the tower-mounted instrument at the same height. After correction for high frequency loss, which amounted to 5% at this low height (it is expected to decrease rapidly with height), the standard deviation of the wind recorded by the sonde agreed to within 2% with that obtained by the reference instrument. A notable result of the field tests is that there was no sign of degradation of the performance of the sonde in strong turbulence conditions. 相似文献
148.
Kjell Billström 《International Journal of Earth Sciences》1991,80(3):717-727
The distribution of sulphur isotope compositions in the Åmmeberg sulphide ore deposit is discussed. The mg src="/content/x7804x59616850t1/xxlarge948.gif" alt="delta" align="BASELINE" BORDER="0">34S values for various sulphides show a complex pattern of fluctuations between isotopic equilibrium and non-equilibrium conditions. This feature as well as the observed variations in the mg src="/content/x7804x59616850t1/xxlarge948.gif" alt="delta" align="BASELINE" BORDER="0">34S values of galena and sphalerite are interpreted to have originated from successive pulses of sulphide-forming solutions. On the basis of geological field criteria and sulphur isotope data, the Ammeberg deposit is considered to be a typical distal mineralization, belonging to the volcanic-exhalative group of ore deposits. The banded structure of the ore, the spatial separation of Pb and Zn and the presence of discrete, persistant ore layers probably relate to the type of convective system that created the mineral-forming solutions and to the various processes taking place when the brines were expelled onto the sea floor.
Zusammenfassung Es wird die Verteilung von Schwefelisotopenzusammensetzungen in der Åmmeberg Sulfidlagerstätte diskutiert. Die mg src="/content/x7804x59616850t1/xxlarge948.gif" alt="delta" align="BASELINE" BORDER="0">34S-Werte für verschiedene Sulfide zeigt ein kompliziertes Schwankungsmuster zwischen Isotopengleichgewichts- und Isotopenungleichgewichtsbedingungen. Dieses Merkmal zusammen mit den beobachteten mg src="/content/x7804x59616850t1/xxlarge948.gif" alt="delta" align="BASELINE" BORDER="0">34S Schwankungen von Bleiglanz und Zinkblende werden dahingehend interpretiert, daß sie ihren Ursprung im anhaltenden Zustrom von sulfidhaltigen Lösungen hatten. Auf der Basis von geologischen Geländebefunden und Schwefelisotopendaten wird die Åmmeberg Lagerstätte als eine typische distale Mineralisation eingestuft, welche zur vulkanisch-exhalativen Lagerstättengruppe gehört. Die gebänderte Struktur des Erzes, die räumliche Trennung von Blei und Zink und die Anwesenheit von gesondert durchziehenden Erzlagen sind zum konvektiven System in Beziehung zu setzen, welches die mineralformenden Lösungen lieferte. Ebenfalls zeigt sich ein Zusammenhang zu den verschiedenen Prozessen, welche abliefen als die Sole auf den Meeresboden ausgestoßen wurde.
Résumé L'auteur discute la distribution des compositions du soufre dans le gisement de sulfure d'Åmmeberg. Les valeurs de mg src="/content/x7804x59616850t1/xxlarge948.gif" alt="delta" align="BASELINE" BORDER="0">34S pour divers sulfures présentent des fluctuations complexes entre les conditions d'équilibre et de non-équilibre isotopique.Cette distribution, ainsi que les variations observées de mg src="/content/x7804x59616850t1/xxlarge948.gif" alt="delta" align="BASELINE" BORDER="0">34S de la galène et de la blende sont interprétées comme résultant d'arrivées successives de solutions sulfurantes. Sur la base de critères géologiques de terrain et des données relatives aux isotopes du soufre, le gisement d'Åmmeberg est considéré comme une minéralisation typiquement distale, appartenant au groupe volcanique exhalatif. La structure rubanée du minerai, la séparation spatiale du Pb et du Zn et la présence de couches de minerai discrètes et continues doivent vraisemblablement être mises en relation avec le type de système convectif qui a engendré les solutions minéralisantes et avec les divers processus qui sont entrés en jeu lorsque les saumures se sont répandues sur le fond de la mer.
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src="/content/x7804x59616850t1/xxlarge1080.gif" alt="icy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1095.gif" alt="chcy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1085.gif" alt="ncy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1099.gif" alt="ycy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1093.gif" alt="khcy" align="BASELINE" BORDER="0"> mg src="/content/x7804x59616850t1/xxlarge1089.gif" alt="scy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1091.gif" alt="ucy" align="MIDDLE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1083.gif" alt="lcy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1100.gif" alt="softcy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1092.gif" alt="fcy" align="MIDDLE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1080.gif" alt="icy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1076.gif" alt="dcy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1086.gif" alt="ocy" align="BASELINE" BORDER="0"> mg src="/content/x7804x59616850t1/xxlarge1074.gif" alt="vcy" align="BASELINE" BORDER="0"> mg src="/content/x7804x59616850t1/xxlarge1091.gif" alt="ucy" align="MIDDLE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1082.gif" alt="kcy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1072.gif" alt="acy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1079.gif" alt="zcy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1099.gif" alt="ycy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1074.gif" alt="vcy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1072.gif" alt="acy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1102.gif" alt="yucy" align="BASELINE" BORDER="0">mg 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src="/content/x7804x59616850t1/xxlarge1103.gif" alt="yacy" align="BASELINE" BORDER="0"> mg src="/content/x7804x59616850t1/xxlarge1079.gif" alt="zcy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1085.gif" alt="ncy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1072.gif" alt="acy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1095.gif" alt="chcy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1077.gif" alt="iecy" align="MIDDLE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1085.gif" alt="ncy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1080.gif" alt="icy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1081.gif" alt="jcy" align="MIDDLE" BORDER="0"> d34S, mg src="/content/x7804x59616850t1/xxlarge1085.gif" alt="ncy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1072.gif" alt="acy" align="BASELINE" BORDER="0">mg 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src="/content/x7804x59616850t1/xxlarge1074.gif" alt="vcy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1080.gif" alt="icy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1085.gif" alt="ncy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1094.gif" alt="tscy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1086.gif" alt="ocy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1074.gif" alt="vcy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1086.gif" alt="ocy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1084.gif" alt="mcy" align="BASELINE" BORDER="0"> mg src="/content/x7804x59616850t1/xxlarge1073.gif" alt="bcy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1083.gif" alt="lcy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1077.gif" alt="iecy" align="MIDDLE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1089.gif" alt="scy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1082.gif" alt="kcy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1077.gif" alt="iecy" align="MIDDLE" BORDER="0"> mg src="/content/x7804x59616850t1/xxlarge1080.gif" alt="icy" align="BASELINE" BORDER="0"> mg src="/content/x7804x59616850t1/xxlarge1094.gif" alt="tscy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1080.gif" alt="icy" align="BASELINE" BORDER="0"> mg src="/content/x7804x59616850t1/xxlarge1085.gif" alt="ncy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1082.gif" alt="kcy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1086.gif" alt="ocy" align="BASELINE" BORDER="0">mg src="/content/x7804x59616850t1/xxlarge1074.gif" alt="vcy" align="BASELINE" BORDER="0">