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12篇 您的检索式:作者名="Gordon EP"
    题名 作者 年代 出处 被引量
1Correlation between β - adrenergic receptors in human lymphocytes and heart 显示文摘Gordon EP Bristow MR Laser JA 1983Circulation1983,68,:1
2Reproducibility of left ventricular volume by two-dimensional echocardiography显示文摘Gordon EP Schnittger I Fitzgerald PJ 1983J Am Coll Cardiol1983,2,:1
3Comparison of plasticity in vivo in the developing visual cortex of normal and protein kinase A RIbeta-deficient mice显示文摘Hensch TK Gordon JA Brandon EP McKnight GS Idzerda RL Stryker MP 1998J Neurosci1998,18,6:1
4Divergent roles for C-type lectins expressed by cells of the innate immune system显示文摘McGreal EP Martinez-Pomares L Gordon S 2004Mol Immunol2004,41,11:1
5Ligand recognition by antigen-presenting cell C-type lectin receptors显示文摘McGreal EP Miller JL Gordon S 2005Curr Opin Immunol2005,17,1:1
6Computerized quantitative analysis of left ventricular wall motion by two-dimensional echocardiography显示文摘Schnittger I Fitzgerald PJ Gordon EP 1984Circulation1984,70,:1
7Cell proliferation in hu- man coronary arteries 显示文摘Gordon D Reidy MA Benditt EP 1990Proc Natl Acad Sci1990,87,:1
8Ligand recognition by antigen- presenting cell C-type lectin receptors显示文摘McGreal EP Miller JL Gordon S 2005Curr Opin Immunol2005,17,1:1
9Soybean goiter 显示文摘Shepard TH Gordon EP Kirschvink JF 1960New Engl J Med1960,262,22:1
10Cell proliferation in human coronary arteries显示文摘 Reidy MA Benditt EP 1990Proc Natl Acad Sci1990,87,:1
11Soybean goiter 显示文摘Shepard TH Gordon EP Kirschvink JF 1960New Engl J Med1960,262,22:1
12Clay Mineralogy and its Paleoclimatic Significance of the OligoceneMiocene Sediments in the Gerze Basin, Tibet显示文摘This study collected the early Oligocene to middle Miocene sediments from the Gerze Basin of Tibet, and used X-Ray diffraction(XRD) and Scanning Electron Microscope(SEM) to discuss their clay mineralolgy, clay indices, better understand the clay mineralogy and its paleoclimatic significance. The results show that clay minerals of the Gerze Basin sediments are mainly composed of illite and chlorite, with minor amounts of smectite and kaolinite, and their relative content varies along the section. Variations of relative contents and clay indices suggest that the Gerze Basin has experienced three-stage evolution of paleoclimate: Ⅰ) high illite and chlorite contents, with fluctuant smectite and low(I+Ch)/(K+S) ratio, indicative of a dominant seasonal arid climate from the early Oligocene to late Oligocene; Ⅱ) higher illite and chlorite contents and larger(I+Ch)/(K+S) ratio but absence of kaolinite, indicating a colder and drier climate from the late Oligocene to early Miocene; Ⅲ) high illite and chlorite contents with fluctuant(I+Ch)/(K+S) ratios and occasional occurrence of kaolinite, suggesting that the climate became warmer and more humid compared with that of stage Ⅱin the mid-Miocene. These conclusions were also reinforced by the clay morphology, which suggests that physical weathering dominated in stage Ⅱ, while relatively strong chemical weathering was dominant in stages Ⅰ and Ⅲ. Clay minerals of the sediments mainly consist of illite and chlorite, indicating that the source rock played a significant role in clay origin. It is inferred that global cooling and the enhancement of denudation and obstruction of northward moisture due to the uplift of the Qinghai-Tibet Plateau were responsible for the provenance of illite and chlorite under weak chemical weathering. Though the Qinghai-Tibet Plateau reached a certain elevation by the mid-Miocene, yet the mid-Miocene widespread warming might have largely impacted the Gerze climate.SONG Eping ZHANG Kexin CHEN Jiangjun WANG Chaowen JIANG Gaolei YIN Ke HONG Hanlie CHURCHMAN Jock Gordon 2014Acta Geologica Sinica(English Edition)2014,88,5:0
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