斑晶的 meaning in Chinese
phenocrystic
porphyrocrystic
Examples
- Analysis for kinetics and deformation of porphyroblasts within ductile shear zones and numerical modeling in large plastic deformation
剪切带中斑晶的运动学和变形分析及塑性大变形计算机模拟 - Some results acquired by computer calculation show that the rigid garnet pophyroblasts can rotate as their matrix flow , and the rotational degree depends on the shear force , ratio of poephroblasts to matrix and the locations of porphyroblasts in the model
计算结果表明：刚性的石榴石斑晶会随着基质的流动而产生旋转运动，旋转量的大小取决于剪切力的大小斑晶的密集度以及斑晶在剪切带中的位置。 - Through the study of the example of shaxi porphyry body in anhui province , the authors first figured out the storage time of plagioclase phenocrysts , then calculated the nucleation rate and growth rate of the crystals and , on such a basis , established the thermal model for cooling of the hypabyssal magmatic system
本文试图通过对安徽沙溪斑岩体进行实例研究，先求出斜长石斑晶的存储时间，再算得晶体成核速率和生长速率，进而建立起浅成岩浆体系冷却的热模型。 - Plastic strain first starts from ambient of the porphyroblast , and then develops to rims of porphyroblast and gradually transfers to the centers of porphyroblasts . the brittle remains in the central parts of porphyroblasts come to be decreased through the plastic deformation development , which is accordance with the banding of intensity in many mylonitization zones on wild occurrences and observation in the fabrics of mylonitization rocks under microscope
长石眼球构造的形成主要是由长石与石英的韧性差决定的，塑性变形首先从斑晶的周围部分开始，逐渐向斑晶发展，脆性残斑核不断减小，这与剪切带内糜棱岩化强度分带相一致。 - The qiongzhong and danxian granites are belong to the kcg - type ( k - rich calc - alkaline ) granitoids according to the tectonic nomenclature by barbarin ( 1999 ) . these foliated kcg - type granites with original orientated structure are the results generated in a changing geodynamic orogenic environment with alternating compressional to extensional stress field . this suggests that hainan island has been a part of south china since latest permian , and been major in extrusion environment of the tethys tectonic system
根据barbarin ( 1999 )分类，琼中和儋县岩基花岗岩属于高k及含钾长石斑晶的钙碱性花岗岩，同时它们具有原生定向构造，是挤压?松弛?挤压的构造演化过程的产物，表明海南岛从二叠纪末期开始已经是华南大陆的一部分，主要受到了特提斯构造域的影响。