Wednesday, January 7, 2009

Minerals


A mineral is a naturally occurring solid, homogeneous substance with a definite chemical composition, and have a specific crystalline structure, a highly ordered atomic structure, and specific physical properties, formed through geological processes.
A rock is an aggregate of one or more minerals. Some rocks are predominantly composed of just one mineral. Other rocks contain many minerals, and the specific minerals in a rock can vary widely.. The vast majority of the rocks of the Earth's crust consist of quartz, feldspar, mica, chlorite, kaolin, calcite, epidote, olivine, augite, hornblende, magnetite, hematite, limonite and a few other minerals.
A main determining factor in the formation of minerals in a rock mass is the chemical composition of the mass, for a certain mineral can be formed only when the necessary elements are present in the rock.
Every year, almost 2000 minerals are discovered. Two types of minerals are usually found by the researchers based on their chemical components. In fact, only a few dozen are common within the rocks of the Earth's crust so it is only a limited number of minerals that you are likely to find in your backyard.
There are many different types of minerals and each type is made of particular types of atoms. The atoms are bonded together and arranged in a special way called a crystal lattice, a network of atoms. The lattice of atoms is what gives a mineral its crystal shape.
Minerals are needed by the body in small amounts to help it function properly and stay strong. Iron, calcium, potassium, and sodium are some of essential minerals. Humans need small amounts of about 14 minerals to maintain normal body function and good health. Read More

Friday, September 5, 2008

Genesa of marble in Trenggalek

1. The existence of the limestone that is happening because of the existence of the limestone that came from the Campurdarat Formation and the Member of the Wonosari Formation that be aged Miosen.

2. Because of the existence of the influence of the pressure (metamorphism because of the influence of the pressure) that is happening because of the limestone unit was in the underside from the Campurdarat Formation afterwards was dealt with by the other rock unit that is by from the Jalen Formation, Formasi Wuni, Formasi Nampol and the Wonosari Formation

3. Because of the influence of the temperature (metamorphism because of the influence of the temperature) that is happening because of the limestone intrusion by the igneous rock and because of the structure of geology (fault/fracture) intensively

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Kaolin

Kaolin merupakan masa batuan yang tersusun dari material lempung dengan kandungan besi yang rendah, dan umumnya berwarna putih atau agak keputihan. Kaolin mempunyai komposisi hidrous alumunium silikat (2H2O.Al2O3.2SiO2), dengan disertai beberapa mineral penyerta.

Proses pembentukan kaolin (kaolinisasi) dapat terjadi melalui proses pelapukan dan proses hidrotermal alterasi pada batuan beku felspartik, mineral-mineral potas aluminium silka dan feldspar diubah menjadi kaolin. Endapan kaolin ada dua macam, yaitu: endapan residual dan sedimentasi.

Mineral yang termasuk dalam kelompok kaolin adalah kaolinit, nakrit, dikrit, dan halloysit (Al2(OH)4SiO5.2H2O), yang mempunyai kandungan air lebih besar dan umumnya membentuk endapan tersendiri.

Sifat-sifat mineral kaolin antara lain, yaitu: kekerasan 2 – 2,5, berat jenis 2,6 – 2,63, plastis, mempunyai daya hantar panas dan listrik yang rendah, serta pH bervariasi.

Potensi dan cadangan kaolin yang besar di Indonesia terdapat di Kalimantan Barat, Kalimantan Selatan, dan Pulau Bangka dan Belitung, serta potensi lainnya tersebar di Pulau Sumatera, Pulau Jawa, dan Sulawesi Utara. Read More
Zlio.com