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427篇 您的检索式:作者名="Eglinton"
    题名 作者 年代 出处 被引量
1应用生物标志化合物参数判识古沉积环境显示文摘本文应用分子有机地球化学方法研究了中国陆相沉积盆地22个代表性样品,试图确认陆相沉积物的古环境。样品包括白垩纪至第三纪的油页岩、页岩、泥岩和芒硝。根据地质和地球化学资料判断,所研究的样品均为湖相沉积物。按盐度可划分为淡水、半咸水或淡水和高盐度水或咸水三种环境的沉积物。对沉积样品抽提物的脂肪烃组分进行了色谱分析和色谱-质谱分析,并在质量色谱图上测得无环烷烃和环烷烃化合物的相对丰度及有关参数。傅家谟 盛国英 许家友 贾蓉芬 范善发 彭平安 Eglinton G.Gowar A.P. 1991地球化学1991,20,1:126
2抚顺烛煤中二甲基一、三甲基-2-甲基-2-(4,8,12-三甲基十三基)色满和苯并藿烷及其地球化学意义显示文摘甲基-2-甲基-2-(4,8,12-三甲基十三基)色满(M-MTTC)的分布与沉积环境有关。在抚顺烛煤中发现5,7,8-三甲基-MTTC和5,8-二甲基-MTTC以及7,8-二甲基-MTTC,不存在一甲基-MTTC。M-MTTC的这种分布反映了抚顺烛煤的淡水滨湖相沉积环境。与此相应的是,抚顺烛煤含有C_(32)—C_(35)苯并藿烷,具有很高的姥鲛烷/植烷比值,高碳数正烷烃的奇偶优势和C_(24)—C_(34)异构烷烃的偶奇优势。范善发 傅家谟 Geoffery Eglinton Simon C.Brassell 1988地球化学1988,17,4:3
3一种可能的煤成油母质——泥炭藓煤的有机地球化学特征显示文摘形成于贫营养型高地沼泽的云南金所泥炭藓软褐煤的链烃主要由正烷烃组成,异戊二烯类烃含量甚低,含少量陆源三萜烯。芳烃馏分主要由三芳,四芳三萜类和两个未知化合物组成。前者具典型陆源输入的奥利烷或乌散烷分子骨架,褐煤Rren^0仅0.24%,但芳构化作用已十分强烈,且芳烃主要由芳构化陆源三萜类组成。傅家谟 盛国英 陈德玉 刘德汉 S. C. Brassell A. Gowar G. Eglinton 1987地球化学1987,16,1:2
4Thermal alteration as a contributory process to the genesis of petroleum显示文摘Henderson W Eglinton G Simmonds P 1968Nature1968,219,:1
5A reassessment of the sources and importance of land derived organic matter in sur face sediments from the Gulf of Mexico显示文摘GONI M A RUTTENBERG K C EGLINTON T I 1998Geochimica et Cosmochimica Acta1998,62,18:1
6Sources of sedimentary lipids deduced from stable carbon isotope analyses of individual compounds 显示文摘Gareth Rieley Robert J Collier David M Jones Geoffrey Eglinton Paul A Eakin Anthony E Fallick 1991Nature1991,352,:1
7Thermal alteration as contributory process to genesis of petroleum显示文摘Henderson W Eglinton G Simmods P 1968Nature1968,209,:1
8Marine and terrestrial biomarker records for the last 35,000 years at ODP site 658C off NW Africa 显示文摘ZHAO M X EGLINTON G HASLETT S K 2000Organic Geochemistry2000,31,9:1
9Vertical and lateral fluid flow related to a large growth fault,South Eugene Island Block 330 Field,Offshore Louisiana显示文摘Losh S Eglinton L Schoell M 1999AAPG Bulletin1999,83,:1
10Biological marker compounds as indicators of depositional history of the Maoming oil shale显示文摘Brassell S C Eglinton G Mo F J 1986Organic Geochemistry1986,10,:1
11Organic geochemical indicators of palaeoenvironmental conditions of sedimentation显示文摘Didyk B M Simoneit B R T Brassell S C Eglinton G 1978Nature1978,272,5650:1
12Lipid chemistry of Icelandic hot spring microbial mats显示文摘Robinson N Eglinton G 1990Organic Geochemistry1990,15,3:1
13Peculiarities of salt lake sediments as potential source rocks in China显示文摘Fu Jiamo Sheng Guoying Peng Pingan Brassell S C Eglinton G Jiang Jigang 1986Org Geochem1986,10,13:1
14The molecularly- uncharacterized component of nonliving organic matter in natu ral environments 显示文摘Hedges J I Eglinton G Hatcher P G 2000Organic Geochemistry2000,31,:1
15Molecular proxies for paleoclimatology显示文摘Eglinton T I Eglinton G 0,,1:1
16Mapping of C4 plant input from North West Africa into the North East Atlantic sediments 显示文摘Huang Yongsong Lydie Dupont Michael Sarnthein John M Hayes Geoffrey Eglinton 2000Geochimica et Cosmochimica Acta2000,64,:1
17Lipid biomarker,δ^13C and plant macrofossil stratigraphy of a Scottish montane peat bog over the last two millennia显示文摘Ficken K J Barber K E Eglinton G 1998Organic Geochemistry1998,28,:1
18Alkanes from plants of the genus Achillea 显示文摘Pal R Eglinton T I Benitez-nelson B C 1999Journal of the Serbian Chemical Society1999,64,78:1
19Surface and subsurface manifestations of gas movement through a N-S transect of the Gulf of Mexico 显示文摘Whelan J Eglinton L etal 2005Marine and Petroleum Geology2005,22,:1
20Lipids of aquatic organisms as potential contributors to lacustrine sediments-II显示文摘Cranwell P A Eglinton G Robinson N 1987Organic Geochemistry1987,11,6:1
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