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1)  anticlockwise P-T-t path
逆时针方向P-T-t轨迹
2)  Clockwise P T path
顺时针P-T轨迹
3)  ACW-IBC P-T path
逆时针近等压降温P-T轨迹
4)  P-T-t path
P-T-t轨迹
1.
The related UHP metamorphic P-T-t path has been reconstructed which could be subdivided into four stages,including prograde(StageⅠ)and UHP metamorphism(StageⅡ)during deep-subduction,and initial quartz eclogite-facies(StageⅢ)and later amphibolite-facies(StageⅣ)retrograde metamorphism during exhumation.
如何建立苏鲁-大别超高压岩石深俯冲-超高压-快速折返过程连续而完整的P-T-t轨迹及精细的年代谱系,是目前地学界研究的热点。
5)  P-T-t paths
P-T-t轨迹
1.
Based on the detail studies of relationship between metamorphism and deformation of Mayuan Group (early Proterozoic) and Mamianshan Group (late Proterozoic)in Northern Fujian and P-T-t paths determinated from the zoned garnets, as well as the data of structural geology and isotopic geochronology, it is proved that the metamorphic rocks of Mayuan Group formed in early Proterozo.
本文通过对闽北麻源群和马面山群变质岩详细的变质变形关系的研究和石榴子石环带测定P-T-t轨迹的应用,结合构造地质和同位素年代学的资料,证实了麻源群变质岩形成于早元古代或更老年代,在早元古代末期遭受过中压、中高温变质,但在晚元古代晋宁期与中元古代形成的马面山群岩石一起经历了强烈的变质变形作用,表现为早元古代麻源群岩石遭受强烈改造,具有早期地壳再活化特点。
6)  p-T paths
p-T轨迹
1.
Medium-low pressure metamorphism and P-T paths in Danba domain, Sichuan province of the western China.;
四川丹巴地区中低压变质作用及P-T轨迹
2.
Metamorphism of continental collisional belts is generally characterized by clockwise p-T paths, especially for those involving isothermal decompression following the pea.
大陆碰撞带变质作用一般以顺时针p-T轨迹演化为特征,尤其伴有峰期变质之后的等温减压过程。
补充资料:提婆五逆与三逆
【提婆五逆与三逆】
 (故事)(参见:五逆)
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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