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1)  Chengde area
承德地区
1.
The sedimentation of Tuchengzi Formation was mainly preserved in Chengde syncline and in the south part of Gubeikou fault in Chengde area, namely Chengde basin and Gubeikou basin, respectively.
承德地区土城子组的沉积地层,主要保存在两个地区,一处为承德向斜,另一处为古北口断层的南部紧邻断层地区,即分别命名的承德盆地和古北口盆地内。
2.
The developing of Chengde Area in modern ages arised under special historic backgrounds.
承德地区近三百年开发是在特殊的历史背景下进行的,关内移民大量出关与塞外政治中心──避暑山庄的出现,对这一地区的近代经济开发起了很大的推动作用,本文以避暑山庄的兴衰为线索,论述了在前后两个开发阶段中这一地区的区域特征与经济开发过程,并指出山庄的衰落不仅影响了承德自身的经济发展而且也影响了整个地区的经济地理面貌。
3.
Fourth-order sequence selected as mapping unit,the lithofacies paleogeography maps of Chengde area were made,based on the sequence stratigraphic framework of Permo-Carboniferous.
将层序地层学方法应用于岩相古地理研究中,首先建立承德地区石炭-二叠系层序地层格架,然后以四级层序为基本编图单元,编制岩相古地理图。
2)  Chengde and Zhangjiakou area
张家口、承德地区
1.
An Ecological Model of interplanting mulberry trees with pasture and farming crops to check wind and control sand was put forward,which was suited for Chengde and Zhangjiakou area of Hebei province.
通过对河北省张家口、承德地区生态环境特点及梯田坝坡种植条桑优点的研究,提出将条桑在张家口、承德地区推广,与牧草、粮等作物间作,形成适宜河北北方的防风固沙高效生态模式。
3)  Chengde Basin
承德盆地
1.
Geochemistry of Dabeigou basalt in Chengde Basin, Hebei Province and constrains on lithospheric mantle thinning of North China Craton;
河北承德盆地114Ma大北沟组玄武岩地球化学及其对华北克拉通岩石圈地幔减薄作用的制约
2.
Geochemistry and Geochronology of Dabeigou Volcanic Rocks in Chengde Basin, Hebei Province and Constrains on Lithospheric Mantle Thinning of North China Craton;
河北承德盆地大北沟组火山岩地球化学和年代学研究
3.
Based on Wang\'s previous studies, this paper focuses on the studies of high Ti content andesites of Dabeigou Group from the Chengde Basin in North China which is first found.
本文通过中国东部承德盆地大北沟组底部高Ti安山岩的研究,在汪方跃研究基础上,进行了更进一步的地球化学分析,包括对承德盆地野外个别样品的重新补采(08CD21,08CD22,08CD23、XYY(仅做辅助对比之用))、锆石U-Pb、Lu-Hf原位微区LA-MC-ICP MS联机分析(08CD21,08CD22,08CD23)、部分样品主量、微量(CD-13、DBG-30、DBG-31、DBG-32、08CD21、08CD22、08CD23、XYY)以及Sr-Nd-Pb同位素(CD-13、DBG-30、DBG-31、DBG-32)的重新测试或补测。
4)  Chengde land block
承德地块
5)  Zhangjiakou and Chengde regions
张承地区
1.
Owing to the special geography location,Zhangjiakou and Chengde regions are endowed with special ecological function.
解决张承地区生态环境问题的关键是解决生态建设与当地经济发展的矛盾。
6)  Baode area
保德地区
1.
Based on measuring the out section,the analysis of inner data,the petrologic character,lithologic association,sedimentary structure, palaeourrent directions,and distribution of sandstone,the sedimentary characters of the Qiaotou sandstone in the Taiyuan formation in Baode area is studied systematically.
对于山西保德地区桥头砂岩的成因,一直存在不同认识。
补充资料:太平洋地区标准会议标准(见太平洋地区标准会议)


太平洋地区标准会议标准(见太平洋地区标准会议)
standards of PASC: see Pacific Area Standards Congress; PASC

Ta iPingyang Diqu Bioozhun Hu呼ib沁幻Zhun太平洋地区标准会议标准(s切md田心sofR巧C)见太平洋地区标准会议。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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