• 河北省平山县阜平套高角门岩相岩石

    The Fuping Group in Pingshan County, Hebei Province, is a suite of high-grade amphibolite-facies rocks.

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  • 中国大陆河北省保定市阜平邮政编码 073200 。

    The postcode of Fuping County, Baoding City, Hebei Province, China is 073200.

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  • 运用景观生态学研究方法分析了阜平土地利用自然景观格局特征

    The characteristics of natural landscape pattern of Fuping County was analyzed with landscape ecological method.

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  • 顶太古界重褶皱位于阜平太古宙穹状复合褶皱一个状褶皱“钩子”部位。

    The Houshiding Archean repeated fold within the Fuping domal composite fold group is located in the "hook" of a "hook-like" fold.

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  • 阜平片麻杂岩湾子层状岩系之间发育大规模角度伸展变形沿变形带南营片麻岩位。

    A large low angle extension deformation belt, along which NYG was emplaced, was found between FPGC and WZLS.

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  • 采用抽样调查收集农田施肥数据结合耕层土壤养分状况,分析阜平主要粮食作物的农田施肥状况和养分结构

    Collecting fertilization data by spot check, combining with the nutrient qualilty of the furrow soil, we analyzed the fertilization and nutrient structure on the food crop farmland of Fuping County.

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  • 依据野外调查资料室内化学分析,组建了阜平表壳的填单元,单元分为阜平表壳岩上部阜平表壳岩下部岩石。

    Based on the field survey and indoor analysis, geological mapping unit for Fuping surface shell rocks is built, and the unit is divided into upper and lower parts.

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  • 1996年在保定市易县、高阳、清苑、阜平、蠡县等地,对大石生长结果适应性果实品质进行了研究。

    The growth, fruit setting, adaptability and fruit quality of Dashi early maturing plum were observed from 1991 to 1996.

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  • 采用土地经济学研究方法土地利用结构、土地利用程度土地利用效益3个方面,对阜平2003年土地资源利用状况进行了对比分析

    Analysis of land utility efficiency in Fuping County was made by economical ways from three aspects including land utility structure, utility degree and efficiency in 2003.

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  • 泰山地区阜平麻岩英云闪长质片麻岩、奥长花岗质片麻岩组成,呈西向带状分布形成于角岩相环境,岩石普遍具片麻状构造,局部地区岩石的韧性作用比较强烈。

    The Fuping-time gneiss in the Taishan area, consisting of tonalite gneiss and trondhjemite, formed in NW zonal distribution in the amphibolite -facies temperature and pressure environment.

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  • 泰山地区阜平麻岩英云闪长质片麻岩、奥长花岗质片麻岩组成,呈西向带状分布形成于角岩相环境,岩石普遍具片麻状构造,局部地区岩石的韧性作用比较强烈。

    The Fuping-time gneiss in the Taishan area, consisting of tonalite gneiss and trondhjemite, formed in NW zonal distribution in the amphibolite -facies temperature and pressure environment.

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