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1.(1) and (2) correspond to a geosynclinal regime with geosynclinal folding and closing (Hercynian), while (3) corresponds to a diwa regime (epi-Hercynian).
在区域大地构造的关系上:①、②对应于地槽褶皱、封闭的地槽体制(海西期),③对应于地洼体制(后海西期)。收藏指正
2.Study on the Late Carboniferous San Li xia reef in Qinling geosynclinal,Shaanxi
陕西秦岭海槽晚石炭世三里峡生物礁研究收藏指正
3.CHARACTERISTICS OF CARBONIFEROUS CRUSTAL MOVEMENTS IN NORTH XINJIANG WITH REFERENCE TO THE TIME OF GEOSYNCLINAL CLOSING
新疆北部石炭纪地壳运动特征兼论地槽区封闭时代收藏指正
4.On the nature of the Devonian biogeographical province of the geosynclinal region in Northern China
北方槽区泥盆纪生物地理区的特征收藏指正
5.From Martin Luther to Descartes:The Relationship between the “Justification byFaith” and the Uprise of Subjective Principle
从马丁·路德到笛卡尔——论“因信称义”与近代主体性哲学兴起的关系收藏指正
6.THE SINIAN STRATIGRAPHICAL SUBDIVISIONS,CORRELATION AND STRUCTURAL HISTORY OF THE KIANGNAN GEANTICLINE IN THE SOUTH CHINA CALEDONIAN GEOSYNCLINAL REGION
华南加里东地槽区江南地背斜带震旦纪地层划分、对比及构造发展问题收藏指正
7.Youfangxi-Erbahuo area is situated in Late Hercynian Nanxingan geosynclinal fold belt and developed with Mesozoic volcanics, strong Yanshanian intermediate-acid magrnatism and a series of volcanic-subvocanic hydrothermal Ag polymetal ore deposits.
摘要内蒙油房一二把伙地区位于华北地台北缘南兴安晚华力西期地槽褶皱带,中生代火山岩系发育,燕山期中酸性岩浆活动强烈,形成了一系列火山、潜火山热液型银多金属矿床。收藏指正
8.As the petrogenetic environment is concerned, the Baimangying covered intrusion was formed by the anatexis of geosynclinal sediments in the upwarping process of south China Caledonian geosyncline which includes south Hunan;
就成岩环境而论,白芒营(宝昌)隐伏岩体是包括湘南地区在内的华南加里东地槽褶皱隆起过程由地槽堆积物通过深熔作用形成的;收藏指正
9.Chronically training weakened the antioxidative function under Se deficiency, resulting in the significant decline of GSH Px/MDA ratio and the significant uprise of MDA content.
低硒状态下长期训练损害了机体抗氧化功能,使 G S H? Px/ M D A 比值显著下降, M D A 浓度显著升高。收藏指正
10.Based on the detailed studies of the basic problems such as the tectonic Framework,tectonic deformation,tectonic metamorphism,the chronology of magmatic,activity,dynamo-thermal,the attribution of the tectonic region,the author recovers the process of tectonic evolution of the Altai geosynclinal orogenic belt.
对阿尔泰山地区的构造格局、构造变质、岩浆岩时代、动力热事件和构造区类型归属等几个地学基础问题进行深入细致研究的基础上,反演了阿尔泰地槽造山带形成和演化的递进历程。收藏指正
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