排序方式: 共有7条查询结果,搜索用时 78 毫秒
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Gear selectivity and the variation of yield 总被引:2,自引:0,他引:2
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Interpretation of in situ target-strength data 总被引:1,自引:0,他引:1
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MacLennan David N; Gerlotto Francois; Masse Jacques 《ICES Journal of Marine Science》2003,60(3):435-436
The ICES Symposium on Acoustics in Fisheries and Aquatic Ecology(SAFAE) was held in Montpellier, France, from 10 to 14 June2002. There were 303 participants from 37 countries, emphasizingthe strongly international character of the meeting. This Symposiumwas the fifth organized by ICES in a series concerned with acousticsin fisheries and related fields. The first two were held inBergen (1973 and 1982), the third in Seattle (1987), and thefourth in Aberdeen 相似文献
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Michael P. Eddy Mauricio Ibaez‐Mejia Seth D. Burgess Matthew A. Coble Umberto G. Cordani Joel DesOrmeau George E. Gehrels Xianhua Li Scott MacLennan Mark Pecha Kei Sato Blair Schoene Victor A. Valencia Jeffrey D. Vervoort Tiantian Wang 《Geostandards and Geoanalytical Research》2019,43(1):113-132
We present multitechnique U‐Pb geochronology and Hf isotopic data from zircon separated from rapakivi biotite granite within the Eocene Golden Horn batholith in Washington, USA. A weighted mean of twenty‐five Th‐corrected 206Pb/238U zircon dates produced at two independent laboratories using chemical abrasion‐isotope dilution‐thermal ionisation mass spectrometry (CA‐ID‐TIMS) is 48.106 ± 0.023 Ma (2s analytical including tracer uncertainties, MSWD = 1.53) and is our recommended date for GHR1 zircon. Microbeam 206Pb/238U dates from laser ablation‐inductively coupled plasma‐mass spectrometry (LA‐ICP‐MS) and secondary ion mass spectrometry (SIMS) laboratories are reproducible and in agreement with the CA‐ID‐TIMS date to within < 1.5%. Solution multi‐collector ICP‐MS (MC‐ICP‐MS) measurements of Hf isotopes from chemically purified aliquots of GHR1 yield a mean 176Hf/177Hf of 0.283050 ± 17 (2s, n = 10), corresponding to a εHf0 of +9.3. Hafnium isotopic measurements from two LA‐ICP‐MS laboratories are in agreement with the solution MC‐ICP‐MS value. The reproducibility of 206Pb/238U and 176Hf/177Hf ratios from GHR1 zircon across a variety of measurement techniques demonstrates their homogeneity in most grains. Additionally, the effectively limitless reserves of GHR1 material from an accessible exposure suggest that GHR1 can provide a useful reference material for U‐Pb geochronology of Cenozoic zircon and Hf isotopic measurements of zircon with radiogenic 176Hf/177Hf. 相似文献
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