| 1. | Lithogeochemistry and lithogenetic epoch for shaba granulite in mianning , sichuan
四川冕宁沙坝麻粒岩的岩石地球化学性质及形成时代 |
| 2. | Granulite - facies retrograde metamorphism of garnet pyroxenite in muzidian , northern dabie mountains
北大别木子店石榴辉石岩的麻粒岩相退变质作用 |
| 3. | The high pressured granulite belts in the xuanhua area of hebei province are very worthy of being studied
河北省宣化地区的高压麻粒岩带是非常具有研究意义的。 |
| 4. | Granulites are the important component of the crust and there are high - pressured granulites generated in many areas of phanerozoic erogenic belts on the earth
麻粒岩是地壳的重要组成部分。全球许多显生宙造山带基地有高压麻粒岩的产出。 |
| 5. | Studies on the metamorphism and ptt path of the granulites now become to be one of the most important methods to module a structural evolvement pattern of erogenic belts
研究高压麻粒岩的变质作用和ptt轨迹已成为建立造山带演化构造模式的最重要途径之一。 |
| 6. | Since eclogite and the coexisting high - pressure granulite have been found in western syntaxis , we ' ll ask whether it is possible that eclogite also can occur in eastern syntaxis
西构造结已经发现榴辉岩和与之共生的高压麻粒岩，东构造结是否也可能存在榴辉岩呢 |
| 7. | The high - pressured granulites are formed both in the convergent area such as the subduction zones and collision zones and in the spreading area such as the bottom of the island arcs
高压麻粒岩既可形成于汇聚型构造环境如俯冲带、碰撞带等，也可形成于伸展型构造环境如岛弧底部。 |
| 8. | High - pressure granulite and the coexisting eclogite and coesite - bearing ultrahigh - pressure eclogite have been subsequently found in the western syntaxis since 80s " last century
自20世纪80年代以来，西构造结已经发现了高压麻粒岩，与高压麻粒岩共生的榴辉岩和含柯石英的超高压榴辉岩。 |
| 9. | Quantitative calculation of trace element content for the residue after partial melting suggests that intermediate - mafic granulites outcropped in the dabie orogen are not the residue of partial melting
残留相微量元素定量计算结果表明，大别山现今出露的中基性麻粒岩不是部分熔融后形成的残留体。 |
| 10. | Lots of information suggest that the metamorphism process of this area are from granulite facies to amphibolite facies and the retrograded metamorphic path is basically a cw nearly isothermal decompressional evolvement trend
各种信息表明本区的变质作用是由麻粒岩相退变到角闪岩相。退变质轨迹基本上是一个顺时针近等温减压型演化趋势。 |
