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mesozoic intrusive
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  中生代侵入
     Nd, Sr, Pb isotopic characteristics of the Mesozoic intrusive rocks in the Taihang-Da Hinggan Mountains Tectonomagmatic Belt and their source region.
     太行山-大兴安岭构造岩浆带中生代侵入岩Nd、Sr、Pb同位素特征及物质来源探讨
短句来源
     ~(40)Ar/~(39)Ar dating of hornblende and biotite in Mesozoic intrusive complex from the North China Block: Constraints on the time of lithospheric thinning
     华北地块中东部中生代侵入杂岩中角闪石和黑云母的~(40)Ar/~(39)Ar定年:对岩石圈减薄时间的制约
短句来源
     Mesozoic intrusive complex in central eastern North China Block (NCB) is mainly composed of two sets of rock associations such as appinite and granodiorite.
     华北地块中东部中生代侵入杂岩存在有富闪侵入岩和花岗闪长岩类两套岩石组合。
短句来源
     Characteristics and zircon SHRIMP U-Pb ages of the Mesozoic intrusive rocks in Fanchang,Anhui Province
     安徽繁昌中生代侵入岩的特征和锆石SHRIMP测年
短句来源
     The Mesozoic intrusive body growing in Suxianshi Jinzhai area of Beihuaiyang stretches at about 150km 2. The intrusive body can be grouped as 3 super units (include 10 units) and 3 independent units based on the intrusive spectra units deviding principle.
     北淮阳金寨—苏仙石地区中生代侵入岩出露面积约150km2,按岩石谱系单位的划分原则,可分为3个超单元(包括10个单元)和3个独立单元。
短句来源
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  中生代侵入岩
     Nd, Sr, Pb isotopic characteristics of the Mesozoic intrusive rocks in the Taihang-Da Hinggan Mountains Tectonomagmatic Belt and their source region.
     太行山-大兴安岭构造岩浆带中生代侵入岩Nd、Sr、Pb同位素特征及物质来源探讨
短句来源
     Characteristics and zircon SHRIMP U-Pb ages of the Mesozoic intrusive rocks in Fanchang,Anhui Province
     安徽繁昌中生代侵入岩的特征和锆石SHRIMP测年
短句来源
     GENETIC RELATIONS BETWEEN MESOZOIC INTRUSIVE AND VOLCANIC ROCKS IN ZHEJIANG
     浙江省中生代侵入岩和火山岩成因关系
短句来源
     GEOCHEMICAL CHARACTERISTICS OF MESOZOIC INTRUSIVE ROCK IN SOUTH JIANGSU PROVINCE
     苏南中生代侵入岩的地球化学特征
短句来源
     Characteristics and Petrogenesis of the Mesozoic Intrusive Rocks in Fanchang, Anhui Province
     安徽繁昌中生代侵入岩的特征和成因研究
短句来源
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  “mesozoic intrusive”译为未确定词的双语例句
     Petrogenesis of the Mesozoic Intrusive Complexes from the Southern Taihang Orogen, North China Craton: Elemental and Sr-Nd-Pb Isotopic Constraints
     太行山南段中生代杂岩体的岩石成因:元素和Nd-Sr-Pb同位素地球化学证据
短句来源
     K2O content of Mesozoic intrusive magmatic rocks in Yanshan innercontinental orogeny is correlated statistically with crust depth( H), with a statistic linear equation wk2o=0. 374+0.101 H, which is different from that of island irc volcanoes in plate margines.
     燕山北区中酸性侵入岩K2O含量普遍较高,平均为5.0%,而燕山南区中酸性侵入岩K2O含量平均为4.0%。 统计分析表明,燕山陆内造山带中生代中酸性侵入岩氧化钾与地壳厚度呈线性相关,相关直线方程为wk20=0.374十0.101H;
短句来源
     K_2O SPATIAL DISTRIBUTION OF MESOZOIC INTRUSIVE MAGMATIC ROCKS AND ITS CORRELATION WITH THE CRUST DEPTH
     中酸性侵入岩氧化钾平面分布规律及其与地壳厚度的关系
短句来源
     SPATIAL DENSITY DISTRIBUTION OF MESOZOIC INTRUSIVE ROCKS AND A BRANCH OF MENTLE INTRUSIVE ROCK DENSITY AND A BRANCH OF MANTLE PLUME IN NORTHERN HEBEI PROVINCE
     冀北地区中生代岩浆岩密度分布特征及其幔枝构造的研究
短句来源
     Mesozoic Intrusive Magmatism-Related Metallogenetic System in Beichagoumen Area
     北岔沟门中生代岩浆侵入作用成矿系统
短句来源
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  mesozoic intrusive
A geochemical and isotopic study was carried out for three Mesozoic intrusive suites (the Xishu, Wu'an and Hongshan suites) from the North China Craton (NCC) to understand their genesis and geodynamic implications.
      
Petrogenesis of the Mesozoic intrusive complexes from the southern Taihang Orogen, North China Craton: elemental and Sr-Nd-Pb is
      
Petrology, element and isotopic geochemistry of the Mesozoic intrusive rocks in the Tongling area were systematically investigated in this study.
      
Petrogenesis of the Mesozoic intrusive rocks in the Tongling area, Anhui Province, China and their constraint on geodynamic proc
      


In Zhejiang province. Mesozoic intrusive rocks and widespread volcanic rocks are closely associated in space. Their time of formation is close and their petrochemical and geochemical characteristics are similar. It is inferred that they are the products formed by cognate magmas different environments. The author discusses the genetic relations in the above-mentioned aspects.

浙江省内中生代侵入岩与大面积分布的火山岩,在空间上密切共生,形成时间相近,岩石化学、地球化学特征相似,推测它们系为同源岩浆在不同环境下形成的产物。

By summing up the minerogenic features of Mesozoic intrusive rock system,it stands to reason that the system belongs to a calc-alkaline rock series of highly differentiated type,with high diagenetic temperature and oxygen fugacity.The rock series has also an enrichment mineralization potential of sulphophile elements.In the light of minerogenesis of the Xiaoxinancha Cu-Au deposit,the geneticrelationship between the deposit and the Mesozoic intrusive rock series and the physico-chemical pro-cess of...

By summing up the minerogenic features of Mesozoic intrusive rock system,it stands to reason that the system belongs to a calc-alkaline rock series of highly differentiated type,with high diagenetic temperature and oxygen fugacity.The rock series has also an enrichment mineralization potential of sulphophile elements.In the light of minerogenesis of the Xiaoxinancha Cu-Au deposit,the geneticrelationship between the deposit and the Mesozoic intrusive rock series and the physico-chemical pro-cess of the minerogenesis are analysed.

文中总结了中生代侵入岩系的成矿作用特征;得出了该岩系为强分异型钙碱性岩石系列,成岩温度和氧逸度较高,具有亲硫型元素富集成矿潜势的认识。从小西南岔铜金矿床成矿作用,分析其与中生代侵入岩系的成因联系,并研究了成矿作用的物理化学过程。

Widely distributed Mesozoic innercontinental orogeny has caused the intrusion of several hundreds of magmatic bodies in Yanshan Area where the K2O content of Mesozoic in trusive magmatic rocks decreases gradually from the north to the south and from the west to the east.K2O content of Mesozoic intrusive magmatic rocks in Yanshan innercontinental orogeny is correlated statistically with crust depth( H), with a statistic linear equation wk2o=0. 374+0.101 H, which is different from that of island...

Widely distributed Mesozoic innercontinental orogeny has caused the intrusion of several hundreds of magmatic bodies in Yanshan Area where the K2O content of Mesozoic in trusive magmatic rocks decreases gradually from the north to the south and from the west to the east.K2O content of Mesozoic intrusive magmatic rocks in Yanshan innercontinental orogeny is correlated statistically with crust depth( H), with a statistic linear equation wk2o=0. 374+0.101 H, which is different from that of island irc volcanoes in plate margines. This equation provides quantitative information for sttldying palaeostructures of mantle-crust border surface in continental Yenshan Area.

燕山地区中生代陆内造山作用强烈,形成数百个中生代中酸性侵入体。本区侵入岩(wsio2为60%~76%)的氧化钾分布具有南北分区、东西分带的特征。燕山北区中酸性侵入岩K2O含量普遍较高,平均为5.0%,而燕山南区中酸性侵入岩K2O含量平均为4.0%。统计分析表明,燕山陆内造山带中生代中酸性侵入岩氧化钾与地壳厚度呈线性相关,相关直线方程为wk20=0.374十0.101H;地壳厚度是决定燕山地区中生代侵入岩氧化钾空间分布的主要因素,与板块边缘岛弧带火山岩氧化钾空间分布的主要制约因素明显不同。

 
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