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岩石碎裂

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In which a mix of water and chemicals is blasted underground to create fissures in gas-bearing rocks.

这种技术的原理是,通过水和化学物的混合物在地底的爆炸使蕴藏有天然气的岩石碎裂

These rocks are lack of foliation and resulted from the brittle fragmentation of mineral grains with rotation of grain fragments accompanied by fractional grain boundary sliding and dilatancy.

这类岩石缺乏面理构造,是由于矿物颗粒的脆性碎裂,旋转以及颗粒边界的磨擦滑动和扩展而造成的。

These rocks are lack of foliation and resulted from the brittle fragment ation of mineral grains with rotation of grain fragment s accompanied by fractional grain boundary sliding and dilatancy.

这类岩石缺乏面理构造,是由于矿物颗粒的脆性碎裂,旋转以及颗粒边界的磨擦滑动和扩展而造成的。

Dues to the regional dynamometamorphism, the rocks formed a narrow string structural zone of strong plastic deformsation and plastic flow and occur different degree rock of cataclasite mylonite, phyllonite etc.

岩石由于经受区域动力变质,形成强烈塑性变形和塑性流动的线性狭长构造带,产生不同程度的碎裂岩,糜棱岩及千糜岩等岩石。

When the fault throw is relatively small, the shale gouge ratio and clay smear potential are relatively large and shale smear is strong. In addition, the coal layers on both sides of the fault are mainly juxtaposed against shale. Therefore, shale smear and juxtaposition play a key role in the sealing. In contrast, when the fault throw is relatively large and shale smear is relatively weak, juxtaposition is unfavorable for sealing. However, the mylonite resulted from strong cataclasis can act as a seal of the coals. The cementation resulted from underground water activity is of great significance to the sealing ability of the fault. Mylonitic coal layers resulted from faulting occur on both sides of the fault. They are unique reservoirs with low permeability and high displacement pressure and their scales depend, to some extent, on the fault throw, fault properties, the hanging wall and footwall.

结果表明:①当断层落差较小时,断层泥比率和泥岩涂抹潜势值较大,泥岩涂抹效应强烈,且与断层两侧煤层对接的岩石主要为泥岩类,此时起封闭作用的主要为泥岩涂抹作用和断层两侧岩性配置关系;②当断层落差较大,泥岩涂抹作用较弱时,对接越不利于封闭形成,但碎裂作用强烈,沿断层两侧形成的糜棱岩对煤层起到了封闭作用;③地下水活动导致的胶结作用对整个断层的封闭具有重要的意义;④断裂作用形成的糜棱煤沿断层两侧分布,此糜棱煤带是一种低渗透、高排替压力的特殊储层,其规模与断层的落差、性质、上下盘都有一定关系。

This fracturing of rock has already begun!

这种岩石的碎裂已经在发生了!

The ductile extension shearing between rock layers is the main structure action, which causes the plastic fludization and mylonization of rocks during the later period of late proterozoic era, and the brittle-ductile extension shearing is the main cause to form the breccias and quartz veins during Yenshan movement.

首次提出了金山韧性剪切带伸展—逆冲—伸展剪切的多阶段发展演化模式。晚元古代晚期的顺层韧性伸展剪切是形成金山地区岩石塑性流变和强烈糜棱岩化的主要构造作用,燕山运动期迭加的脆—韧性伸展剪切是形成该地区碎裂岩和石英脉的主要构造作用

Frictional experiments using a self-designed "multifunction servo friction and abrasion experiment machine" with the multi-parameter synchronous data collection system and online data processing software have been made on six types of rocks. The analyses of the experiments results indicate that earthquake faults with large displacement bring up a series of products continually changing from cataclasis to melting. The rocks contained mafic minerals are easier to melt and the gas bubbles in melting products proved the hydroxy water from the minerals has participated the rock melting process and decreased the melting point of the rock. Frictional melting is more sensitive to speed than normal stress. The temperature sharply increases at about 40℃/sec when the sample enters the earthquake fault state. While the melting happens, torsion decreases instantly and there is perhaps a "blind region" of normal stress.

利用自行设计加工的&多功能伺服摩擦磨损实验机&,及多参数同步数据采集系统和联机数据处理软件,对六类岩石进行的实验和分析成果表明:大位移地震断层作用形成了与滑动速率有关的从碎裂到熔融连续变化的系列产物;含镁铁质矿物的岩石更容易熔融,熔融产物中出现的气泡证实了矿物羟基水很可能参与了岩石的熔融过程并降低岩石熔点;相对于正应力而言摩擦熔融程度对速度变化更加敏感;此外,进入地震断层状态时温度急剧上升达~40℃/秒;伴随熔融发生出现扭矩骤减时,可能存在一个短暂的正应力&盲区&。

Within the rock, there are some angular shaped, randomly arranged fragments which make up 50% of the entire rock. This fault rock is called cataclasite.

就以这一块标本为例,在岩石中有含量为50%的棱角状岩屑,岩屑排列无序,这块断层岩被称为碎裂岩。

Within the rock, there are some angular shaped, randomly arranged fragment s which make up 50% of the entire rock. This fault rock is called cataclasite.

就以这一块标本为例,在岩石中有含量为50%的棱角状岩屑,岩屑排列无序,这块断层岩被称为碎裂岩。

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In the negative and interrogative forms, of course, this is identical to the non-emphatic forms.

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