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1)  Alay Basin
阿拉伊盆地
1.
Petroleum geological characteristics and resource potential of Alay Basin in Central Asia;
中亚地区阿拉伊盆地石油地质特征及勘探潜力
2.
Analysis of Tectonic Geology and Petroleum-Bearing Conditions in Alay Basin, Central Asia
中亚地区阿拉伊盆地构造地质特征与油气条件分析
2)  Artala Basin
阿尔塔拉盆地
1.
Study on metallogenic conditions and prospecting direction of sandstone type uranium deposits in Artala Basin, Inner Mongolia;
内蒙古阿尔塔拉盆地砂岩型铀矿成矿地质条件及找矿方向初探
3)  Yili basin
伊犁盆地
1.
Structure and fluid evolution of Yili basin and their relation to sandstone type uranium mineralization;
伊犁盆地盆山构造演化及流体演化与砂岩型铀矿成矿的关系
2.
Influences of Zhahe fault on hydrogeological conditions of deposit No.511 at the southern margin of Yili Basin;
扎河断裂对伊犁盆地南缘511矿床水文地质条件的影响
3.
Geological characteristics and metallogenic mechanism of No. 511 sandstone-type uranium ore deposit in Yili basin,Xinjiang;
新疆伊犁盆地511砂岩型铀矿床成矿作用机理研究
4)  the Yitong Basin
伊通盆地
1.
Lots of subaqueous gravity flow sedimentary bodies were developed in the Eocene strata of Chaluhe Fault Depression,the Yitong Basin.
伊通盆地岔路河断陷始新统中发育大量水下重力流沉积,根据重力流发育位置及沉积特征,可划分为浅水浊流沉积、深水浊流沉积、水下滑塌沉积和水下泥石流沉积4种类型。
2.
The Caluhe Depression of the Yitong Basin is a extension rift basin,due to the complex tectonics,particular morphology,sedimentary source from several directions,several depocenter and subsidence center and the rapid facies transition,there is much difficulty in the stratigraphic division and correlation.
伊通盆地岔路河断陷属于伸展断陷盆地,由于其复杂的构造作用、独特的几何形态、多物源供应、具多个沉积沉降中心以及侧向相变快的特点,给地层划分和对比带来了很大的困难。
5)  Yitong basin
伊通盆地
1.
Characteristics and Hydrocarbon Generation-Expulsion Histories of Source Rocks in Moliqing Rift of Yitong Basin;
伊通盆地莫里青断陷烃源岩特征及生排烃史
2.
Diagenesis of reservoir of the Shuangyang Formation of Paleogene in Moliqing Faulted Depression of Yitong Basin, Jilin Province;
吉林伊通盆地莫里青断陷古近系双阳组储层成岩作用研究
3.
Study of Eocene lithologic traps in Chaluhe fault depression of Yitong Basin;
伊通盆地岔路河断陷始新统岩性圈闭研究
6)  Ili Basin
伊犁盆地
1.
REE geochemistry of sandstone-type uranium deposit in interlayer oxidation zone in the southern margin of Ili Basin,Xinjiang;
新疆伊犁盆地南缘层间氧化带砂岩型铀矿床中稀土元素地球化学特征
2.
Super-enriching Mechanism of Disperse-elements Re and Se in Interlayer Oxidation——A Case Study of the Zhajistan Interlayer Oxidation Zone Sandstone-type Uranium Deposit, Ili Basin, Xinjiang;
层间氧化带分散元素铼与硒的超常富集机制探讨——以伊犁盆地扎吉斯坦层间氧化带砂岩型铀矿床为例
3.
Depositional system of the Lower-Middle Jurassic Shuixigou Group in the western segment of the southern margin of the Ili basin and its controls on uranium mineralization;
伊犁盆地南缘西段中下侏罗统水西沟群沉积体系及其对铀成矿的控制作用
补充资料:伊本·阿拉比
伊本·阿拉比(1165~1240)
Ibn al-‘Arabī

   
伊斯兰教神秘主义哲学家。生于西班牙的穆尔西亚。早年就学于塞维利亚和休达,深受两名女苏非的影响。1194年他到突尼斯。1201年赴麦加朝觐,接着游历伊拉克和安纳托利亚,最后定居大马士革。他将思辨的苏非主义发展为系统的神秘主义理论体系,归结为“存在的单一”。他认为,真主是绝对的存在,一切存在的本原。万物以观念形式预先存在于真主的认识中,通过照明而显现,并按同样方式复归;观念的原型是世界万物与绝对存在的中介,真主的超在性和内在性,是人得以认识真主的依据;理性的宇宙原则,即穆罕默德的实在,最充分的表现是完人;完人是宇宙一切完美属性的缩影,是世界存在的理由和复归的保证。他的主要著作《麦加的默示》和《智慧的珍宝》,通过伊本·法里德、阿塔尔、鲁米等人传遍伊斯兰世界,为整个苏非派的发展提供理论框架。他死于大马士革。被后人尊为大长老和宗教复兴者。
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