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Imex Marmol Dominicana - Marble * Granite * Construction Materials

Welcome to Imex Mármol's Website.

 

We are a proud group of professionals dedicated to the importation and sales of Marble, Granite and Construction Materials for the dominican market. In the present, we offer our products with headquarters in Santo Domingo and Santiago, Dominican Republic.

 

With the new implementation of our website, " Imex Marmol . Com ", we'll try to expand our current market, in the same way that we have expanded our catalog this year, including construction materials such as water resistant roof tiles and rebars. You'll find any information from these products in our online catalog, still in the process of creation. Wich we'll try to have ready as soon as possible. We'll do all that is necessary to satisfy our dominican market, the construction materials sector in specific.

 

You will be able to find the necessary means to get in contact with us in the Contact page, in the event that you want information currently not available online, or even broader information about products you do see in this site.

 

Our Best Regards;

 

Imex Mármol's Team.

Santo Domingo & Santiago, Dominican Republic.

 

 
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La Pizarra

 

La pizarra es una roca metamórfica homogénea formada por la compactación de arcillas. Se presenta generalmente en un color opaco azulado oscuro y dividida en lajas u hojas planas siendo, por esta característica, utilizada en cubiertas y como antiguo elemento de escritura.

  

Last Updated on Thursday, 04 February 2010 17:36
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Marble

 

Background

The word marble comes from the Greek word marmaros which means shining stone. To the geologist, marble is a non-foliated, granular metamorphic rock that is formed by the metamorphism of limestone and dolostone. It is usually formed by regional metamorphism but sometimes is formed by contact metamorphism. Both limestone and marble are calcium carbonate (CaCO3) which is also the composition of the mineral calcite. The metamorphism of limestone causes the calcite grains to grow in size and to interlock with one another. The result is that marble is noticeably more dense and harder than limestone. Limestone frequently contains invertebrate fossils. However, these fossils are almost always destroyed by metamorphism..

 

Last Updated on Friday, 02 October 2009 12:08
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