precede 发表于 2025-3-30 09:49:48
Garnet Orientation in Different Metamorphic faciesby the preferred orientation of omphacite, quartz and calcite, too..The results partly agree with Kamb’s (1959) calculation for cubic minerals: or [ 111 ] parallel to the main compression direction.他姓手中拿着 发表于 2025-3-30 13:58:10
http://reply.papertrans.cn/32/3190/318974/318974_52.png移植 发表于 2025-3-30 19:26:07
http://reply.papertrans.cn/32/3190/318974/318974_53.png柏树 发表于 2025-3-30 23:37:45
http://reply.papertrans.cn/32/3190/318974/318974_54.pngDEFER 发表于 2025-3-31 02:40:34
http://reply.papertrans.cn/32/3190/318974/318974_55.png注入 发表于 2025-3-31 08:48:23
https://doi.org/10.1057/9781137412591e quartz-diagrams show a distinctive preferred orientation of poles of prism-planes a (1120) and m (lOlO), namely, am-girdle. At the part of the highest metamorphic grade the diagrams show almost nearly single one-crystal-fabrics through the positions of sub-planes of quartz. The mechanism of quartz-orientation was also discussed.ADORN 发表于 2025-3-31 09:29:36
Global Business Value Innovationsmade by simply combining the appropriate anisotropy coefficients with area-corrected pole density data obtained from the contour values of . distributions, and standard calculated intensities for the given material. Calculated and observed diffraction patterns for apatite in tibia of . and for calcite in Yule marble are in good agreement.ABIDE 发表于 2025-3-31 13:45:22
https://doi.org/10.1007/978-3-658-11867-9n Polfigur. Sie liefert den Texturzustand von Proben in so kurzer Zeit, daß es damit möglich ist, Untersuchungsprogramme auch großen Umfangs schnell abzuwickeln oder laufende Produktionskontrollen so schnell durchzuführen, daß man noch in den Fertigungsprozeß eingreifen kann.意外的成功 发表于 2025-3-31 18:42:44
http://reply.papertrans.cn/32/3190/318974/318974_59.pnglandfill 发表于 2025-3-31 21:47:35
Röntgenographische Gefügeanalyse von Quarzschiefern aus Zentral-e quartz-diagrams show a distinctive preferred orientation of poles of prism-planes a (1120) and m (lOlO), namely, am-girdle. At the part of the highest metamorphic grade the diagrams show almost nearly single one-crystal-fabrics through the positions of sub-planes of quartz. The mechanism of quartz-orientation was also discussed.