1)  distribution
东缘
2)  eastern Tibet
青藏东缘
1.
Study on petrology and mineral chemical compositions of deep-derived mafic enclaves from high-K igneous rocks in Liuhe-Xiangduo area, eastern Tibet showed that the enclaves belong to metamorphic rocks formed in the mid-lower crust.
　对青藏东缘新生代六合 香多地区高钾岩系中镁铁质深源包体的岩石学和矿物化学成分的详细研究表明:六合 香多镁铁质深源包体为中 下地壳变质岩。
2.
The mineral assemblages of spinel-lherzolite xenoliths in Maguan Area, Eastern Tibet are Ol+Opx+Cpx+Spl.
青藏东缘马关尖晶石二辉橄榄岩包体的矿物组合为橄榄石 (Ol) +斜方辉石 (Opx) +单斜辉石 (Cpx) +尖晶石 (Spl)。
3.
Thermochronological studies suggest that two types of high-potassic magmatism occur in eastern Tibet and the time of igneous activities corresponds to 40-28 Ma and 16-0 Ma, respectively.
热年代学研究表明 ,青藏东缘存在两期新生代高钾岩浆活动 ,其活动时限分别为 40～ 2 8Ma和 16～ 0Ma。
3)  eastern marginof Songliao basin
松辽东缘
4)  east edge rupture
东缘断裂
5)  eastern margin of the Dabie Mountains
大别山东缘
1.
The 40Ar/39Ar ages of the muscovite samples T28-12 and T28-13 from mylonite of the earlier Tan-Lu ductile shear belt on the eastern margin of the Dabie Mountains are (181.
大别山东缘早期郯庐韧性剪切带内的T28-12和T28-13白云母的(181。
2.
On the basis of calculation for temperatures and pressures experienced by the two phases of the fault zone as well as the thermo-chronological information of mylonite from the earlier and later Tanlu fault zones on the eastern margin of the Dabie Mountains, this paper discusses the delamination history and uplifting magnitudes of the Dabie Mountains from earlier J.
郯庐断裂带与大别造山带在大别山东缘相复合 ,并将大别—苏鲁造山带左行错开达 5 0 0km。
6)  eastern margin of Pamir
帕米尔东缘
参考词条
补充资料：法缘﹝齐﹞（东官曾成）《比丘尼传》卷三
【法缘﹝齐﹞（东官曾成）《比丘尼传》卷三】
法缘。本姓仑。东官曾成人也。宋元嘉九年。年十岁。妹法彩年九岁。未识经法。忽以其年二月八日俱失所在。经三日而归。说至净土天宫见佛。佛为开化。至九月十五日又去一旬乃还。便能作外国书语及诵经。见西域人言谑善相了解。十年正月十五日又复失去。田中作人见其随风飘飏上天。父母忧之祀神求福。既而经月乃返。返已出家披著法服持发而归。自说见佛及比丘尼。语云。汝前世因缘应为我弟子。举手摩头发自堕落。为立法名大名法缘。小曰法彩。临遣还曰。可作精舍。当与汝经。法也缘等还家即毁神座缮立精庐。昼夜讲诵。夕中每有五色光明。流泛峰岭有若灯烛。自此以后容止华雅音制诠正。上京讽诵不能过也。刺史韦朗孔默并屈供养。闻其谈说甚敬异焉。因是土人皆事正法。年五十六。建元中卒也。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。