| 1. | Study on the external cultural influence on chinese architecture from the liu s manor
从大邑刘氏庄园看外来文化对中国建筑的影响 |
| 2. | Manor , liu of dayi
大邑刘氏庄园 |
| 3. | Persisting in scientific development view to push on the urban and rural unification in dayi
坚持科学的发展观推进大邑城乡一体化发展 |
| 4. | But i started to feel very guilty when i saw hundreds of cute little live rabbits at ren xuping ' s farm in dayi county , 50 kilometers away from chengdu
但当我在距离成都50公里的大邑县任旭平的农场里，看到几百只可爱小兔子，我仍旧感到强烈的罪恶感。 |
| 5. | Entering from dayi county , it takes a few days to pass through the original forest of the xiling snow mountain , then you can get to the big snow resevoir and the nerve center
登山线路从大邑进去，穿过西岭雪山原始森林走4天可到达海拔4900米的大雪塘山下的大本营。 |
| 6. | The present longmenshan foreland basin lies between the longmenshan thrust belt and the longquanshan fault . the dayi conglomerate at the bottom of the chengdu basin , although people of the past having studied a certain degree , hasn " t same sugest
大邑砾岩的地质时限为上新世-早更新世，时代界定在4 . 6ma - 0 . 82ma之间，显示该区第三纪与第四纪之间是连续沉积的，其间不存在构造事件。 |
| 7. | 5 ) quantitative analysis to the dayi conglomerate in the cenozoic longmenshan foreland basin has been carried out . the results indicate that the dextral strike - slip rate is 1 . 02 mm / a , the average sedimentary rate is 0 . 143 mm / a , and the average decline rate is 0 . 3mm / a
5 )对新生代前陆盆地大邑砾岩作定量分析，结果表明，大邑砾岩沉积时期，前陆盆地滑移量为1 . 02mm a ，沉积速率为0 . 143mm a ，平均沉降速率为0 . 3mm a 。 |
| 8. | 2 ) analyses and researches systematicly the lithofacies , sedimentary facies and depositional environment of the dayi conglomerate in the cenozoic longmenshan foreland basin . this paper analyzes detailed six coarse elastics lithofacies , five mid - elastics lithofacies and three fine elastics lithofacies . establishes the association of three depositional environment types including alluvial fan and river
2 )对新生代龙门山前陆盆地大邑砾岩岩相、沉积相和沉积环境进行了系统分析和研究，划分出6种粗碎屑岩相、 5种中碎屑岩相、 3种细碎屑岩相，确定了大邑砾岩为冲积扇相、河流相沉积环境的组合。 |
| 9. | 3 ) according to the dayi conglomerate " s gravel composition and direction when water flowed during geological age , comeback the paleogeograph of the longmenshan foreland basin , speculates that the dayi conglomerate " material source is located in the songpan - ganzi fold belt to the east , the pengguan fault to the west of the western sichuan plateau region
3 )根据大邑砾岩砾石成分及古流向分析，推测大邑砾岩物源区为松潘-甘孜褶皱带以东、彭灌断裂以西的龙门山地区，并恢复大邑砾岩沉积时期岩相古地理，认为大邑砾岩物源主要来自龙门山冲断带一侧。 |
