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Jingdezhen Ceramic Institute and Professor Lv Jinquan that they rely on the well-known in Jingdezhen porcelain, teaching emphasis on china clay, the traditional ceramic art research and identification, as well as new media and new technology development, the students after graduation can be inherited the ancient traditional techniques, but also make corresponding innovation.

景德镇陶瓷学院教授吕金全,他们依赖于著名的景德镇瓷器,教学重点放在了中国粘土,传统陶瓷艺术的研究和鉴定,以及新媒体,新技术的发展,学生毕业后可以被继承古老的传统技术,而且还做出相应的创新。

The main types of clay minerals are illite, smectite, kaolinite and chlorite.

粘土矿物主要由伊利石、蒙皂石、高岭石和绿泥石组成。

Chondrite standardized modes of REE show that LREE is richer than HREE in both laterite-type and Carlin-type gold deposit. Carl...

红色粘土型金矿形成于上新世,卡林型金矿形成于白垩纪,在成矿时代上有先后顺序关系。

So it is a reliable approach for the total amount of clay in clastic reservoir rocks.

可作为求取沉积岩储层中粘土总量的可靠方法。

I want to learn how to model clay.

我想学习如何模塑粘土

Then they added clay to create a model of the dinosaur.

然后他们加上粘土就制出了一个恐龙的模型。

WORK HINTS 1 finish the clay model down to the smallest detail.

制作提示 1。完成粘土模具的最小细节 2。

But I fancy I should succeed better if I had some clay or wax to model.

但是我异想天开,我若有粘土或蜡在手,我兴许就将之塑造出来。

Use clay to make a model ..

粘土捏成高山、河流、湖泊的模型。

The main reasons I would I say are behind this are residual model clay left over transfering to the cast part.

主要的原因我想我这样说是背后的是残余粘土模型遗留下来转移到演员的一部分。

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Finally, according to market conditions and market products this article paper analyzes the trends in the development of camera technology, and designs a color night vision camera.

最后根据市场情况和市面上产品的情况分析了摄像机技术的发展趋势,并设计了一款彩色夜视摄像机。

Only person height weeds and the fierce looks stone idles were there.

只有半人深的荒草和龇牙咧嘴的神像。

This dramatic range, steeper than the Himalayas, is the upturned rim of the eastern edge of Tibet, a plateau that has risen to 5 km in response to the slow but un stoppable collision of India with Asia that began about 55 million years ago and which continues unabated today.

这一引人注目的地域范围,比喜马拉雅山更加陡峭,是处于西藏东部边缘的朝上翻的边框地带。响应启始于约5500万年前的、缓慢的但却不可阻挡的印度与亚洲地壳板块碰撞,高原已上升至五千米,这种碰撞持续至今,毫无衰退。