1) the southeastern margin of the Dabie mountains
大别山东南缘
1.
The foreland basin in the southeastern margin of the Dabie mountains experienced an evolution of marine sedimentation-marine-continental sedimentation-continental sedimentation and characterized by superimposed-composited pattern.
大别山东南缘前陆盆地经历了由海相—海陆过渡相—陆相的演化历程,具有复合叠合盆地特征。
2) 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。
3) The southeast foot of Dabie Mountains
大别山东南麓
4) southern margin of the Dabie-Sulu orogenic belt
大别-苏鲁造山带南缘
1.
Tectonic evolution characteristics of the foreland basin on the southern margin of the Dabie-Sulu orogenic belt;
大别-苏鲁造山带南缘前陆盆地演化特征
5) the southern margin of Qinling-Dabie Orogenic Belt
秦岭-大别造山带南缘
6) the southern margin of East Qinling-Dabie orogenic belt
东秦岭-大别造山带南部
补充资料：大别山
| 大别山 位于中国湖北省、河南省、安徽省交界处。东南西北走向。西接桐柏山，东为张八岭，三者合称淮阳山。长江、淮河的分水岭。长 270 千米，褶皱断块山。主峰天堂寨，海拔1729米，位于湖北省罗田县东北；白马尖（一称霍山），海拔1774米，位于安徽省霍山县南。山地被断层分割成许多菱形断块，东南侧黄梅到桐城一带，山麓线挺直，山坡陡到50°以上，是明显的断层崖。山地南北侧修建了许多水库，有梅山、佛子岭、白莲河等水库。原来森林葱郁，但遭长期破坏，覆盖率低，水土流失严重，水库淤塞严重。现存森林以马尾松、杉、栎为主。大别山区是中国茶叶主产区，其中皖西六安瓜片、豫南信阳毛尖、鄂东北的汉绿都是有名的品种。板栗、油桐、油茶、乌桕、漆树等经济林木在低山丘陵区广布。 |
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参考词条