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articleAbstract=漠河盆地依列克得组潜在烃源岩为一套发育在玄武岩系之间的湖沼相沉积岩系。本文利用多种有机地球化学分析手段,探讨了该套烃源岩的有机质丰度、类型、成熟度及火山岩对该套烃源岩的作用。漠河盆地依列克得组烃源岩有机质丰度较高,优于中侏罗系烃源岩;有机质类型以IIB型为主,考虑到风化作用的影响,该套烃源岩有机质类型可能要优于元素分析的结果;有机质热演化程度比较低,处于刚进入生油门限的低成熟阶段,烃源岩并未受其周围玄武岩的过渡热烘烤作用,指示火山岩浆溢出的古地理环境应为水下湖盆环境。, authors=高红梅1 ,高福红2 ,张月巧3 , authorsList=高红梅;高福红;张月巧, authorCompany=1. 中国石油大学(北京)资源与信息学院;油气资源与探测国家重点实验室,北京 1022492. 吉林大学地球科学学院,长春 1300613. 中国石油勘探开发研究院,北京102249, correspAuthors=null, authorNote=null, correspAuthorsNote=高红梅, copyrightStatement=null, copyrightOwner=null, extLink=null, articleAbsUrl=null, sourceXml=null, magXml=null, pdfUrl=null, pdf=9hGnCOaRvfUMGCn2KNMxmg==, pdfFileSize=648172, pdfExtLink=null, richHtmlUrl=null, mobilePdfUrl=null, reviewReport=null, pdfFirstPage=null, abstractGraph=null, abstractGraphContent=null, abstractVideo=null, citation=null, cebUrl=null, magXmlContent=null, mapNumber=null, fund=null)}, authors=[Author(id=1299147407179149797, tenantId=1146029695717560320, journalId=null, articleId=1242119475617665178, 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科技导报
|研究论文
2010
, 28
(1002) :
81
-85
黑龙江省漠河盆地早白垩世火山岩系烃源岩生烃潜力研究
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高红梅;高福红;张月巧
作者信息
Generation Potential of Source Rocks in Volcanic Series of the Early Cretaceous Period in Mohe Basin, Heilongjiang Province
Affiliations
出版时间: 2010-01-28
文章导航
漠河盆地依列克得组潜在烃源岩为一套发育在玄武岩系之间的湖沼相沉积岩系。本文利用多种有机地球化学分析手段,探讨了该套烃源岩的有机质丰度、类型、成熟度及火山岩对该套烃源岩的作用。漠河盆地依列克得组烃源岩有机质丰度较高,优于中侏罗系烃源岩;有机质类型以IIB型为主,考虑到风化作用的影响,该套烃源岩有机质类型可能要优于元素分析的结果;有机质热演化程度比较低,处于刚进入生油门限的低成熟阶段,烃源岩并未受其周围玄武岩的过渡热烘烤作用,指示火山岩浆溢出的古地理环境应为水下湖盆环境。
漠河盆地
/
依列克得组
/
烃源岩
/
生烃潜力
The Yiliekede Formation source rock in Mohe Basin belongs to limnetic facies and is the development in basaltic seriesin. Based on various organic geochemical analyses, the abundant sources of the organic materials, the type of organic materials, the organic maturity and the influence of volcanic rocks on source rocks are discussed. The results show that the organic materials in the source rock are more abundant than in Jurassic Formation source rocks. Based on the elemental analysis, the organic materials are shown to be dominant in the type of IIB kerogen. Due to the weathering effect, the organic materials may be better than in IIB. The degree of thermal evolution of organic matter is still in a low mature stage, and has just entered the oil generation threshold. The source rocks are not heated seriously by the basalt, which indicates that the environment of the spilling of magma belongs to lake basin.
Mohe basin
/
Yiliekede Formation
/
ource rocks
/
hydrocarbon -generating potential
高红梅;高福红;张月巧.
黑龙江省漠河盆地早白垩世火山岩系烃源岩生烃潜力研究.
科技导报,
2010
, 28
(1002)
: 81
-85
.
.
Generation Potential of Source Rocks in Volcanic Series of the Early Cretaceous Period in Mohe Basin, Heilongjiang Province[J].
Science & Technology Review ,
2010
, 28
(1002)
: 81
-85
.
2010年第28卷第1002期
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文章信息
接收时间:2009-11-19
首发时间:2010-01-28
出版时间:2010-01-28
收稿日期:2009-11-19
修回日期:2009-11-18
https://castjournals.cast.org.cn/joweb/kjdb/CN/1242119475617665178
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2种不同金属材料的力学参数
科 Family 属数 Number of genus 种数 Number of species 占总种数比例 Percentage of total species (%) 属 Genus 种数 Number of species 占总种数比例 Percentage of total species (%) 鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78 小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39 多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39 红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87 小菇属 Mycena 11 5.26 光柄菇属 Pluteus 5 2.39 红菇属 Russula 17 8.13 栓菌属 Trametes 5 2.39
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