中布日扎采石场浮雕(以萨巴利夫采石场为例)

Pavlo Horishnyj, A. Pavelchuk
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The mine floor is bounded by the little changed and worked out northern, western and eastern mine walls, western part of the southern wall and significantly changed eastern part of the southern wall. The quarry has the one overburden and three extraction highwalls. Benches are located between the benches of different levels. Their maximum width is 50 m. At least, the benches of three levels can be traced.\n The heaped relief of the Sabariv quarry is presented predominantly by external sheating dumps of the overburden strata. They do not have a specific location. The dumps are terrace-like and have a shape of elongated embankments. They are located at elevations of 260–271 meters. The height of the dry dump is 10–15 m. The dumps of the overburden strata are recultivated. The forest melioration is carried out throughout the territory. The inner quarry dumps are located on the mine floor. 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引用次数: 0

摘要

摘要27个用于提取建筑材料的活跃采石场位于中波布日吉亚境内。结晶岩(花岗岩、混辉岩、花岗闪长岩、绿帘岩等)采石场占主导地位。此外,还有壤土和较少的采石场。他们集中在中部pobuzhzha的西部,靠近城市Vinnytsia。其中大多数是封闭的阶梯式采石场。水晶岩石的采石场主要是长方形的,有狭窄的工作台和平坦的坑底,没有堆积的浮雕。壤土采石场通常逐渐减少,其中一些采石场目前已不活跃,并设有内部堆肥场。这种采石场的长度为300 - 450米,有一个工作的高墙。采石场部分活跃,覆盖着草皮。这些采石场的长度通常为300 - 350米,有多达2 - 3个高墙,也有外部采石场。Sabariv花岗岩采石场位于Vinnytsia市以南1公里处的南Bug河右岸,经过仔细调查。有用岩石的开采始于1958年。采动采用1个覆岩和3个抽采高壁。采石场最大长度为620米,宽度为370米,深度为54米。抽取工作台长度为14米。采石场有开挖(剥蚀)和堆积(堆积)两种地形形式。开挖地形由底板、上覆岩层台阶和抽采高壁组成。矿井底板的形状接近矩形。它是由采石场的第三生产层组成的,目前正在进行采矿工作,以及第二次开采高壁趾的非实质性部分。矿井底板表面的形状一般是对齐的。矿区底板由北、西、东三段变化不大且已成形的矿体、南矿体西部和变化较大的南矿体东部所围合。采石场有一个覆盖层和三个开采高墙。长椅位于不同楼层的长椅之间。它们的最大宽度为50米。至少,三层的长椅可以被追踪。萨巴里夫采石场的堆积地形主要表现为覆盖层的外部覆岩堆。它们没有具体的位置。这些垃圾场呈梯田状,呈细长的堤防形状。它们位于海拔260-271米的地方。干堆高度为10-15米。覆岩堆积场进行了复植。森林改良在全国范围内进行。内部采石场位于矿井底板上。这样的转储并不普遍,容量也很低。关键词:采石场;矿山救援;挖掘救援;堆积形式;Pobuzhzhia中间。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
RELIEF OF THE QUARRIES OF THE MIDDLE POBUZHZHIA (ON THE EXAMPLE SABARIV QUARRY)
Abstract. The twenty-seven active quarries for the extraction of building materials are located on the territory of the Middle Pobuzhzhia. The quarries of the crystalline rocks (granite, migmatite, granodiorite, charnockite, etc.) are dominant. Also, there are loam and less often sand quarries. They are concentrated in the western part of the Middle Pobuzhzhia, near city Vinnytsia. Most of the them are the type of closed stepped quarries. The quarries of the crystalline rocks are predominantly rectangular in shape with narrow benches of working benches and a flat pit floor without heaped forms of relief. Loam quarries are usually gradually declining, some of them are now inactive having internal sheating dumps. The length of such quarries is 300 – 450 m, with one working highwall. Sand quarries are partially active and covered with turf. The length of these quarries is usually 300 – 350 m, with up to 2 – 3 highwalls, also there are external sheating dumps. The Sabariv granite quarry, located 1 km south of city Vinnytsia on the right bank of the Southern Bug River is carefully surveyed. The extraction of useful rocks dates back to 1958. Mining is carried out by one overburden and three extraction highwalls. The maximum length of the quarry is 620 m, width – 370 m, depth – 54 m. The length of extraction benches is 14 m. The quarry has the excavated (denudation) and heaped (accumulative) forms of relief. The excavated relief consists of a mine floor, benches of the overburden stratum and extraction highwalls. The mine floor has a shape close to the rectangle. It is made of the third production horizon of the quarry where currently the mining works are carrying out and of the insubstantial part of the second extraction highwalls toe. The shape of a surface of the mine floor is generally aligned. The mine floor is bounded by the little changed and worked out northern, western and eastern mine walls, western part of the southern wall and significantly changed eastern part of the southern wall. The quarry has the one overburden and three extraction highwalls. Benches are located between the benches of different levels. Their maximum width is 50 m. At least, the benches of three levels can be traced. The heaped relief of the Sabariv quarry is presented predominantly by external sheating dumps of the overburden strata. They do not have a specific location. The dumps are terrace-like and have a shape of elongated embankments. They are located at elevations of 260–271 meters. The height of the dry dump is 10–15 m. The dumps of the overburden strata are recultivated. The forest melioration is carried out throughout the territory. The inner quarry dumps are located on the mine floor. Such dumps are not widespread and have low capacity. Key words: quarry; mining relief; excavated relief; heaped forms; Middle Pobuzhzhia.
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