1.
The ultrabasic rocks form a complex of large tectonic slices with intercalated slices of Sebakwian sedimentary rocks.
超基性岩与塞巴奎沉积岩岩片相间构成一巨大的构造岩片的杂岩体。
2.
PROTEROZOIC TECTONIC SLICES ALONG THE NORTHERN MARGIN OF NORTH CHINA PLATE
华北板块北缘活动带元古宙构造岩片
3.
Garnet glaucophane blueschist from Pana:implications to Tibetan tectonic evolution
旁那石榴蓝闪片岩特征及其构造意义
4.
Research on Structural Character and Deforming Conditions about Tectonic Schist of Xiamaling Formation, Southern of Fangshan Pluton;
房山岩体南侧下马岭组构造片岩构造特征及变形条件研究
5.
Rocks to the north and south of the gneiss zone are lithologically and structurally distinct from it.
片麻岩带南北两侧的岩石，在岩性上及构造上都和它大不相同。
6.
Structure of Metamorphic Rock and Deformation ?
变质岩构造及变形构造
7.
Foliated fault rocks are characterized by well-developed foliation which is resulted from the preferred orientation of mineral grains in the rock.
片理化断层岩石具有发育良好的面理构造，这些面理是岩石中矿物颗粒优选定向而造成的。
8.
Geochemistry of Gneissic Alkaline Granites in Donghai County, Jiangsu Province, and Its Tectonic Significances
江苏东海片麻状碱性花岗岩的地球化学及其构造指示意义
9.
PETROCHEMICAL AND METAMORPHIC STUDY OF QUARTZITE(SCHIST) IN INDUS-YARLUNG TSANGPO TECTONIC ZONE,NAMCHE BARWA,TIBET
南迦巴瓦峰地区雅鲁藏布构造带中石英(片)岩的岩石化学特征及变质条件探讨
10.
schistose structure
【地质】片状构造, 层状结构
11.
TECTONIC AND MAGMAIC EVOLUTION OF THE ARCHEAN GRANITTIC ROCKS IN JILIN PROVINCE
吉林太古宙花岗岩类构造─岩浆演化
12.
I think the foliation is resulted from deformation. The original composition of the foliated rock is granite.
我认为岩石中的这些片理是由于岩石变形造成的，片理化岩石的原岩就是花岗岩。
13.
The gross physical character of a rock or rock formation.
岩性一种岩石或岩石构造的所有物理属性
14.
According to the researchresult, the tectonite consists of mylonite and cataclasite in the fracture zone.
断裂带的构造岩以糜棱岩和碎裂岩为主。
15.
Petrotectonic of Huangling Granite Batholith, Western Hubei;
鄂西黄陵花岗岩岩基岩石大地构造学研究
16.
MESOZOIC-CENOZOIC TECTONIC MAGMATIC PORTFOLIO ANALYSIS IN CUOQIN AREA OF THE MIDDLE GANGDISE
冈底斯构造岩浆带中段措勤地区中新生代岩浆岩构造组合分析
17.
Strong foliation, stretching lineation, a-type folds, sheath folds and mylonite, these structural characteristics only reflect macroscopic evidence.
强烈的片理、拉伸线理、a型褶皱、鞘褶皱以及糜棱岩，这些构造特征仅仅反映出宏观的证据。
18.
X-radiography has sometimes been used with success to detect bedding structures and bioturbation in apparently uniform sandstone.
X射线照片有时已成功地用来发现外表均一的砂岩中的层次构造和生物扰动。