strong clay

strong clay

Pure clay that is essentially free of any other substance.
References in periodicals archive ?
This strong clay enables one to dig approximately 10 kg at one time and the clay source is located nearly an hour walk from Nanga Sumpa.
This could be ascribed to the huge surface area and large aspect ratio of clay sheets dispersed at the nanometer level, which contributes to the strong clay network as shown in Fig.
Holes FCL 005 and FCL 006 intercepted uranium mineralization in the sandstone and strong clay hematite and chlorite alteration, in the basement rocks.
Third seed Ivan Ljubicic made a strong clay court season debut yesterday with a straight-sets win over Spanish wild card Guillermo Garcia-Lopez in the first round of the Valencia Open.
With this strong clay, his mother could make pots that would last a long time.
Yoshida said the larger pipe is made of a strong clay, and the smaller pipe is made of iron.
However the distribution of gold values within the oxide zone also suggests that substantial modification of the original gold distribution as well as secondary depletion and enrichment of gold occurred during the period of intense Tertiary deep weathering that produced the strong clay alteration and oxidation.
Porcelain is an exceptionally strong clay medium that has a strong history, defined by composition, firing results and by the name that describes it.
A coupling agent between clay and polymer is particularly required in polyolefins-based systems to achieve good clay dispersion and strong clay matrix interactions.
The first sample was collected from a four foot channel across a shear zone exhibiting strong clay alteration with visible lead-zinc-pyrite veinlets, which assayed 0.
From a depth of 10ft on, the hole intersected strong hydrothermal alteration with alternating vertical zones of silification and quartz veining, and wide zones of very strong clay alteration.
Porphyry-style, sheeted, flat-lying quartz veins and stockworks associated with strong clay alteration zones within granitic intrusions lying along the north margin of the deformation zone.