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サンプルの注文は1個だけで、包装は簡単に見えますが、簡単ではありません。 梱包はシンプルに見えますが、簡単ではありません。良い仕事。

積み込みの前に入念な清掃と消毒を行い、その後積み込みと補強を行う。私たちはすべてのステップに注力しています。

今、装飾はますます精巧になり、多くの人は石英の装飾を選ぶ。人造石は天然石の高貴で優雅な特徴を保持し、華やかな色彩と均一な色彩の特徴がある。石英を設置する環境は異なるので、環境要因に基づいて選択すべきである。天然仕上げの石英で装飾する部分が異なるので、使用する石英の種類も異なる。屋外の建物の装飾に使用する場合、風、雨、水の季節の太陽に耐える必要がある。御影石は炭酸塩を含まないので、吸水性が低く、耐候性が強い。様々な石英を選択するのが一番です；ホールの場合、床装飾用の単板石英は安定した物理的、化学的性質と高い機械的強度が要求されるので、花崗岩石英を第一選択とすべきです；壁のスカートと家庭の寝室の床の場合、機械的強度がやや劣るので、美しい模様の大理石を使うべきです。

Granite is an intrusive rock in acidic magmatic rock. This is the most common type of rock in this category. Most of it is light flesh red, light gray, and off-white. Medium-coarse, fine-grained structure, block structure. There are also patchy structures, spherical structures, gneiss-like structures and so on. The main minerals of granite are quartz, potash feldspar and acid plagioclase, and the secondary minerals are biotite, hornblende, and sometimes a small amount of pyroxene. The content of potash feldspar is generally more than that of plagioclase. The relationship between the two contents is often that potash feldspar accounts for two-thirds of the total feldspar, plagioclase occupies one-third, and potash feldspar is more in granite. It is light flesh red, but also gray and gray. Off-white potash feldspar and plagioclase are often difficult to distinguish on hand specimens. At this time, we must carefully observe the double crystal characteristics of these two feldspars, because plagioclase has double crystals. When rotating the hand specimens, we can see that there are regular light and dark aggregates on the plagioclase crystals. It is a cassette double crystal, which appears as two halves of crystals with different degrees of brightness. Granite can be further named ...

Put a drop of ink on the back of the marble. If the ink quickly disperses and leaches everywhere, it means that the particles inside the marble are loose and the quality is poor; but if the ink drops do not penetrate, the marble is dense and the quality is good. This is actually a simple test of the water absorption rate of the marble. If the ink droplets do not penetrate, it may indicate that the texture of the marble is relatively dense and the water absorption rate is low. Marble is generally coated with a protective agent to prevent stains from penetrating. Even if the customer sees that the ink droplets are not penetrating, it is likely that the protective agent is working, not the performance of the marble itself. In addition, if the water on the back of the marble becomes bead-like, it means that it is difficult to absorb water after the protective agent is applied to the marble, and it may not be able to adhere to the cement. Therefore, it can be considered that the lower the water absorption on the front of the marble, the better, but it is also It should be ...

Marble is mainly composed of calcite, limestone, serpentine and dolomite, and its main component is calcium carbonate, which accounts for more than 50%. Others include magnesium carbonate, calcium oxide, manganese oxide and silicon dioxide. Marble is generally soft in nature, which is relative to granite. Of course, you don't need to bother about this, because this geological age is calculated in billions. In our lifetime, this marble qualitative change is a limited change. Marble floor tiles have attracted the attention of consumers with their gorgeous appearance and very practical features. The difference between marble and other architectural stones is that each marble floor tile has a different texture. The marble with clear and curved texture is smooth and delicate, bright and fresh, like a visual feast that brings you time and time again, and is installed in the living room. , Can set off the living room more elegant and generous. Because marble generally contains impurities, and calcium carbonate in the atmosphere is affected by carbon dioxide, carbides, and water vapor, it is also easy to weather and dissolve, and the surface of the marble quickly loses its luster.

大理石はもともと、雲南省大理で産出される黒い模様の入った白い石灰岩を指す。その断面は、天然の水墨山水画を形成することができる。古来、大理石は形のある模様で、絵画の屏風やモザイク画によく使われていた。その後、大理石という名称は次第に様々な色や模様を持つものすべてを指すようになり、大理石は石灰岩として建築装飾材に使われるようになった。一般的には白い大理石を白大理石と呼ぶが、西洋で作られる彫像用の白大理石も大理石と呼ばれる。大理石の名前については、かつて我が国大理の大理石が最高品質であったという言い伝えがある。だからこの名前がついた。

研磨後の大理石はとても美しい。大理石は主に建築物の壁、床、台、柱など様々な形や板に加工され、モニュメント、塔、彫像などの記念碑的建築物の材料としてよく使われる。大理石はまた、美術工芸品、文房具、ランプ、器具などの実用的な芸術作品に彫刻することもできる。大理石の分類によって、命名の原則は異なる。丹東緑、鉄嶺赤など、産地と色にちなんだものもあれば、白雪姫、艾葉青など、模様と色にちなんだものもある。大理石には、白大理石、水晶墨玉などの伝統的な名前がある。そのため、大理石の産地が異なるために、似たような名前や、同じ名前の違う石がしばしば現れる現象がある。

Marble is a metamorphic rock formed by the high temperature and high pressure of the original rocks in the earth's crust. The internal force of the earth's crust promotes the qualitative change of various types of rocks. The change of marble quality refers to the change in the structure, structure and mineral composition of the original rock. The new type of rock formed by the marble qualitative transformation is called metamorphic rock. Marble is mainly composed of calcite, limestone, serpentine and dolomite, and its main component is calcium carbonate, which accounts for more than 50%. Others include magnesium carbonate, calcium oxide, manganese oxide and silicon dioxide. Marble is generally soft in nature, which is relative to granite. Of course, you don't need to bother about this, because this geological age is calculated in billions. In our lifetime, this marble qualitative change is a limited change. Marble floor tiles have attracted the attention of consumers with their gorgeous appearance and very practical features. The difference between marble and other architectural stones is that each marble floor tile has a different texture. The marble with clear and curved texture is smooth and delicate, bright and fresh, which is like a visual feast ...