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鄂尔多斯盆地东部马家沟组岩盐元素地球化学特征及成因分析
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鄂尔多斯盆地东部马家沟组岩盐元素地球化学特征及成因分析
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Elemental Geochemical Characteristics and Cause of Formation Analysis of the Rock Salt in Majiagou Formation, East Part of Ordos Basin
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出版时间: 2013-06-18 doi: 10.3981/j.issn.1000-7857.2013.17.009
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为了明确鄂尔多斯盆地东部马家沟组岩盐的地球化学特征和成因,本文通过对碳酸盐岩C、O、Sr同位素及微量元素进行分析和研究,发现研究区内δ13C介于-0.346%~0.108%之间,Sr同位素比值明显较低,Sr/Ba比值均大于1。稀土元素总体上呈现轻稀土元素相对富集,重稀土元素相对亏损的特征。单元素Ce具有微弱的正异常,Eu具有明显的负异常,Sr/Cu比值均大于10,V/(V+Ni)值总体介于0.7~0.8之间。认为该区在马四、马五段沉积期气候干旱炎热,水体较深,处于还原环境,为典型的海相沉积环境,且岩盐在沉积的过程中有可能受到了幔源物质的影响。
地球化学特征  /  成因  /  岩盐  /  马家沟组  /  鄂尔多斯盆地东部
In order to define the geochemical characteristics and cause of formation for the rock salt in the Majiagou Formation, east part of Ordos Basin, C, O, and Sr isotopes and trace elements of carbonate rocks are analyzed and studied. The results show that δ13C concentration is between -3.46‰ and 1.08‰, isotope ratios of Sr are significantly low, the ratio between Sr and Ba is generally bigger than one, LREE is enriched more than HREE, Ce has a weak positive anomaly, Eu has an obvious negative anomaly, and the ratio between V and (V+Ni) is between 0.7 and 0.8. Experimental results indicate that since the climate is dry and hot, the water is deep, and the depositional environment is reductive and marine, the depositional process of rock salt is affected by mantle derived materials.
geochemical characteristic  /  cause of formation  /  rock salt  /  Majiagou Formation  /  east part of Ordos Basin
王伟力;孙莹. 鄂尔多斯盆地东部马家沟组岩盐元素地球化学特征及成因分析. 科技导报, 2013 , 31 (17) : 51 -57 . DOI: 10.3981/j.issn.1000-7857.2013.17.009
WANG Weili;SUN Ying. Elemental Geochemical Characteristics and Cause of Formation Analysis of the Rock Salt in Majiagou Formation, East Part of Ordos Basin[J]. Science & Technology Review, 2013 , 31 (17) : 51 -57 . DOI: 10.3981/j.issn.1000-7857.2013.17.009
2013年第31卷第17期
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doi: 10.3981/j.issn.1000-7857.2013.17.009
  • 接收时间:2012-11-30
  • 首发时间:2013-06-18
  • 出版时间:2013-06-18
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  • 收稿日期:2012-11-30
  • 修回日期:2013-03-27
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2种不同金属材料的力学参数

Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)

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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