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The geology of the Piedmont includes schist, amphibolite, gneiss, migmatite, and granite while the primary resource of the Coastal Plain is kaolin.

地质的皮埃蒙特包括片岩,角闪岩,片麻岩,混合岩和花岗岩的主要资源的海岸平原的高岭土。

Oxygen isotope temperatures of the eclogite mineral-pairs are cumulated at two peak values of 600 to 640℃ and 380 to 430℃, respectively, corresponding to retrograde reequilibration at greenschist-facie and high amphibolite-facies conditions; the peak eclogite-facies temperatures of 750 to 800℃ cannot be retrieved due to the strong retrograde alteration.

石马和黄镇榴辉岩的矿物对氧同位素温度均给出两个峰值: 380~430℃与绿片岩相变质条件一致,600~640℃与高角闪岩相变质条件一致;给不出峰变质温度(750~800℃)是由于岩石经历了退变质流体的强烈改造作用。

Below 1100℃, the amount of argon released from irradiated samples is in an order of: plagioclase rock>striped migmatite>granite>garnetiferous mica schist>calciummuddy shale>basalt.

在1100℃之前,辐照样释放的氩气量按顺序排列为:斜长岩>条带状混合岩>花岗岩>含石榴石云母片岩>钙泥质页岩>玄武岩。

Nalati tectonic belt located between the Ili Basin and the South Tianshan of western Tianshan is 25 km wide, and it is composed of earlier Proterozoic schist, gneiss, migmatite, and migmatitic granite.

那拉提构造带位于天山西段伊犁盆地与南天山之间,出露宽度约 2 5 km,由早元古代片岩、片麻岩及混合岩、混合花岗岩组成;深层次韧性剪切带及叠加中-浅层次剪切带发育;那拉提构造带南缘断裂明显,南侧为古生代浅变质黑色岩系;构造带北缘韧/脆性剪切带宽度大,两侧岩石劈理化后易于混淆,故界线不明显。

When the mechanism of the mylonite is chiefly recrystallization, the rock can be subdivided into phyllonite, structuralschist and structural gneiss on the basis of crystallization and crystal grain size.

机制以重结晶作用为主的糜棱岩可根据结晶程度和结晶颗粒的大小可分为千糜岩、构造片岩和构造片麻岩。

The magmatism of Yanshan period caused wide magmiting, the tectonic sealing obscured the primary mylonite.

燕山期的岩浆热活动,在造山带轴部产生广泛的混合岩化,构造热愈合使糜棱岩转化为构造片岩

Heilongjiang mélange distributed in Yilan area of Heilongjiang Province is regarded as the tectonic mélange with features of suture zone. Some metam orphic basic lavas consisting of quite a few metamorphic minerals without directional characteristics are named massive blue schist.

黑龙江省依兰地区分布的黑龙江杂岩被认为是具有缝合带性质的构造混杂岩,其中所含变基性火山熔岩中含有的变质矿物不具有定向组构特征,因此称之为块状蓝片岩

The main rock types are two mica quartz schist and plagioclase amphibole schist.

老湾金矿床赋矿围岩是经历过多次韧脆性剪切改造作用的中元古界龟山组变质岩系,主要岩石类型为二云石英片岩和斜长角闪片岩

The Zhangbaling schists in the ductile detachment deformation belt are widely mylonitized under low greenschist facies.

韧性滑脱变形带内的张八岭群片岩,广泛发生了低绿片相背景下的糜棱岩化。

The rock is thick-bedded and fresh and occurs as tectonic slices in garnet-bearing mica-quartz schist.

岩石新鲜,带宽500~600m,呈构造岩片产在含石榴子石云母石英片岩中。

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