1) Xinhuatun pluton
新华屯岩体
1.
The whole rock and mineral Rb-Sr isotopic dating suggests that the Xinhuatun pluton located in Zhangguangcailing of Northeast China was emplaced in Middle Jurassic with isotopic ages of 160～165Ma, rather than belonging to Indosinian.
全岩－矿物的锶同位素研究结果表明，出露在张广才岭花岗岩带上的新华屯岩体属中侏罗世晚期的产物，其同位素年龄为１６０～１６５Ｍａ，表明该晶洞花岗岩体不属于印支期。
2) Huashan batholith
华山岩体
1.
Apatite minerals separated from samples that were collected from elevations of 520m to 1 950m on the Huashan batholith, yielded fission track ages of (20 59±3 6)Ma to (29 26±3 3)Ma.
对采自华山岩体不同高度的磷灰石样品进行裂变径迹分析 ,所得结果结合相关地质资料认为 :(1)华山岩体抬升至少始于渐新世或始新世 ;(2 )华山主峰及北峰间可能发育一条对应于华山山前断裂的次级正断层 ,断距约 340m ;(3)据华山北峰样品研究 ,其各时段的平均抬升速率依次为2 9 2 6～ 2 5 0 5Ma ,V =0 183mm/a ;2 5 0 5～ 2 3 2 7Ma ,V =0 152mm/a ;2 3 2 7～ 2 0 59Ma ,V =0 0 19mm/a。
3) Tunchang area metabasites
屯昌地区变基性岩体
4) Tonghualing intermediate-acid intrusive rocks
铜华岭岩体
1.
Tonghualing intermediate-acid intrusive rocks is located in Yemaquan arc between Armantai fault and Kelameili fault,Eastern Junggar,North Xinjiang.
6 Ma,说明铜华岭岩体是早古生代岩浆活动的产物,为东准噶尔早古生代造山带演化提供了花岗岩证据。
5) Yangxin rock mass
阳新岩体
1.
For the first time, we have tried two-dimensional interpretation of electrical sounding in northwestern sector of the Yangxin rock mass and achieved good re-sults.
我们首次在阳新岩体西北段进行了电测深二维解释的尝试,并取得了较好效果。
6) Xinli-village
新立屯
1.
On the analysis of the residence planning and design of Xinli-village and the concrete treatise of the natural corridor and the huma.
通过对本溪市新立屯居住区的规划设计,探讨廊道的组织方法和的城乡廊道网络结构的建设方法。
补充资料：紧屯屯
1.方言。形容非常紧密。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条