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16篇 您的检索式:作者名="Thorseth"
    题名 作者 年代 出处 被引量
1Enumeration of 这rchaea and bacteria in seafloor basalt using real-time quantitative PCR and fluorescence microscopy 显示文摘Einen J Thorseth IH Ovreas L 2008Fems Microbiol Lett2008,282,2:1
2Diversity of life in ocean floor basalt 显示文摘Thorseth I H Torsvik T Torsvik V 2001Earth and Planetary Sci- ence Letters2001,194,:1
3Comparison of iron isotope variations in modern and Ordovician siliceous Fe oxyhydroxide deposits显示文摘Kirsten Moeller Ronny Schoenberg Tor Grenne Ingunn H. Thorseth Kerstin Drost Rolf B. Pedersen 2014Geochimica et Cosmochimica Acta2014,,:1
43-D seismic interpretation using the coherency cube: An example from the South Embra Precaspian Basin, Kazakhstan 显示文摘Thorseth J Riley G 1997the Leading edge1997,16,6:1
5Alteration of ocean- ic volcanic glass: textural evidence of microbial activity显示文摘Fisk M R Giovanoni S J Thorseth I H 1998Science1998,281,:1
6Assessment of Erythemal UV Level in Nepal Based on Solar UV Estimates from Total Ozone Mapping Spectrometer显示文摘Nepal lies on the southern slope of Himalaya in Asia. In a width ranging between 150 and 250 km, the altitude varies greatly from about 100 m at its southern border to a maximum of 8848 min the northern part. Like the variation in altitude, climatic condition varies quite a lot. Long-term monthly mean erythemal UV daily dose values for Nepal are evaluated using Total Ozone Mapping Spectrometer (TOMS) estimation from the time of its overpass between 1996 and 2003. The results are presented as summer and winter maps of mean UV levels in each satellite grid. The mean winter erythemal UV daily dose ranges between 2.1 and 3.6 kJ m-2 whereas summer values are found to lie between 4.6 and 9.7 kJ m-2. The altitude variation increases the UV levels by about 0.2 kJ km-1 in winter months, and 0.9 kJ km-1 in summer. A multiyear monthly average erythemal daily dose in most of the areas shows that the summer value is about three times higher than that in winter. Although year-to-year variation is not pronounced in high- and mid-elevation regions, UV levels seemed to decrease from 1997 to 2002 in the southern part of the country in the low elevation region by about 5.35%. Due to the combined effects of the altitude, low ozone concentration in the troposphere, and thin air, surface UV radiation at higher altitudes is found to be higher than in the surrounding regions.Binod Kumar BHATTARAI Berit KJELDSTAD Trond Morten THORSETH 2011Advances in Atmospheric Sciences2011,28,4:1
7Diversity of life in ocean floor basalt 显示文摘Thorseth l H Torsvik T Torsvik V 2001Earth and Planetary Science Letters2001,194,:1
8Enumeration of Archaea and Bacteria in seafloor basalt using eal-time quantitative PCR and fluorescence microscopy 显示文摘Einen J Thorseth IH +vre2ts L 2008FEMS Microbiol Lett2008,282,2:1
9ROV exploration of the Kolbeinsey Ridge: preliminary results of the SUBMAR-99 cruise 显示文摘Pedersen R Kelly D Thorseth I 1999InterRidge News1999,8,:1
10Alteration of oceanic volcanic glass:textural evidence of microbial activity显示文摘 Giovannoni S J Thorseth I H 1998Science1998,281,:1
11Alteration of oceanic volcanic glass: Textural evidence of microbial activity显示文摘Fisk M R Giovannoni S J Thorseth I H 1998Science1998,281,:1
12Barite in hydro- thermal environments as a recorder of subseafloor processes: A multiple-isotope study from the Loki's Castle vent field显示文摘Eickmann B Thorseth I H Peters M 2014Geobiology2014,12,4:1
13The extent of microbial life in the volcanic crust of the ocean basins显示文摘Fisk M R Giovannoni S J Thorseth I H 1998Science1998,281,:1
14Microbial alteration of 0~30-Ma seafloor and sub-seafloor basaltic glasses from the Australian Antarctic Discordance显示文摘Thorseth I H Pedersen R B Christie D M 2003Earth and Planetary Science Letters2003,215,:1
15Enumeration of Archaea and Bacteria in seafloor basalt using real-time quantitative PCR and fluorescence microscopy 显示文摘Einen J Thorseth I H Ovre s L 2008FEMS Microbiology Letters2008,282,2:1
16利用相干体进行三维地震解释实例:哈萨克Ember Precaspian盆地南部的一个实例显示文摘相干测定相邻记录道的相似性,记录道越相似,相干性越高。例如,横穿断层面的记录道相似性减小,横穿断层的三维时间切片显示低相干值。 Precaspian盆地下、中三叠统沉积层由泥岩、砂岩和砾岩的互层组成,颜色从褐色到淡红很容易识别。上三叠统到下侏罗统地层颜色从灰到淡绿的砂岩与页岩互层。由于很相似,因此,很难从下三叠中分出三叠。整个三叠统到下侏罗统地层超复。构造升高。Jay Thorseth 李彦兰 1998吐哈油气1998,3,4:0
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