阴山英男之: kageyama hideo no iq teacher ds - kangaeru chikara to oboeru chikara
Example Sentences:
1.
Journal of chengdu university social science edition 阴山学刊自然科学版
2.
Kageyama method correct kanji dictation japan version Ds阴山法电脑反覆正确汉字默书日本版
3.
On the position and establishment of the brand of yinshan culture 阴山文化的定位与品牌塑造
4.
A study on hardseededness and bourgeon characteristic of lespedeza inschaniea schindl 阴山胡枝子种子硬实与萌发特性研究
5.
A new investigation into the source of chinese characters and the expounding of yinshan rock painting 汉字源头新探兼阴山岩画解谜
6.
Analysis on the relationship between soil desertffication and character of climate in the north of inner mongolia 阴山北部土地荒漠化与气候特征分析
7.
On the basis of the types of sand stone , light and heavy mineral associations , planimetric map of sedimentary facies and directions of palaeoflow , it is considered that detrital material of terrigenous deposit of chang6 - 8 oil - beds in this area come from southwest provenance , northeast provenance , west provenance and south provenance , respectively , which are the denudation area of huating - longxian county in southwestern , yinshan ancient land in the northern , the denudation area of yantong mountain and tongxin to the west of yangjiajuzi - yinjiacheng county and qinling ancient land in the southern 根据砂岩类型、轻、重矿物组合、沉积相带平面展布及古水流方向等特征的分析，认为研究区延长组长6 ? 8油层组陆源碎屑物质来自西南、东北、西部和南部四大物源区，分别为西南华亭?陇县一带剥蚀区，北部阴山古陆，西部的杨家咀子、殷家城以西的烟筒山、同心地区剥蚀区和南部秦岭古陆。
8.
Rb - sr whole rock - minerals ages determination indicates that the isochronal ages are 25018 ma and 213 . 09 . 8 ma for suhaitu and wenduerhao intrusion , respectively . the dated isotopic ages demonstrate that the alxa alkaline - rich intrusive rocks belong to indosinian alkaline magma activity . the similarities and differences of the alkaline - rich intrusive rocks distributed in the alxa fault block and those distributed along the northern margin of the north china block and the tarim block are compared and discussed 采用rb - sr法对阿拉善断块有代表性的苏亥图温都尔浩富碱侵入岩体的年进行了测定，分别获得25018 ma和213 . 09 . 8 ma的年值，提供了属于印支期的年代学证据，认为阿拉善断块北缘富碱侵入岩和华北断块北缘燕辽阴山印支期富碱性侵入岩带应该划归同一印支期富碱性侵入岩带。
9.
The north provenance provided main detrital material , which can be delicately divided into two different sections , taipusiqi , ji ' ning area in the east and zha ' ertai mountain , wula mountain in the middle of yinshan ancient land . the distribution of gas pool in the eastern part of ordos area was obviously controlled by sedimentary facies belts 北物源区提供了主要的碎屑物质，它又可细分为东、西两个不同的部分，分别为阴山古陆东部太仆寺旗、集宁地区和阴山中部的渣尔泰山、乌拉山地区。
10.
On the basis of the analyses of peripheral ancient land , types of sand stone , light and heavy mineral associations and directions of palaeoflow , it is considered that detrital material of terrigenous origin of the upper palaeozoic in this area come from south provenance and north provenance , respectively , yinshan ancient land in the northern and east qinling ancient land in the southeastern 根据盆地周缘古陆、砂岩类型、轻、重矿物组合及古水流方向等特征的分析，认为研究区上古生界陆源碎屑物质来自南、北两大物源区，即北部的阴山古陆和东南部的东秦岭古陆。
