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pisolitic

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pisolitic

[¦pī·zə¦lid·ik]
(petrology)
Pertaining to pisolite or to the characteristic texture of such a rock.
McGraw-Hill Dictionary of Scientific & Technical Terms, 6E, Copyright © 2003 by The McGraw-Hill Companies, Inc.
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References in periodicals archive
The production boost from 24 to 32 Mt/y will allow the company to take advantage of increases in the international iron ore market for its particular product - pisolitic limonite sinter fines.
This is pisolitic (rounded gravels), iron-enriched, dehydrated bauxite which is cemented into a hardcap layer in places.
Prior to chemical analysis, all soils were air-dried and sieved (<2 mm) to remove stones and pisolitic bauxite.
The 100% owned Riley Iron Ore Mine (Riley DSO Hematite Project) is located 10 km from the Mount Lindsay Deposit and occurs as a hematite rich pisolitic and cemented laterite.
Breuning-Madsen H, Awadzi TW, Koch CB, Borggaard OK (2007) Characteristics and genesis of pisolitic soil layers in a tropical moist semi-deciduous forest of Ghana.
* The petrographic and XRD results of the lithofacies-I indicated oolitic / pisolitic texture of laterite/ bauxite / kaolinite.
- Resource occurs at surface in the form of pisolitic laterite (ref photo)
The intact lateritic profile was mostly formed by weathering of granitoids and other rock types and these profiles commonly consist of sand and pisolitic gravels over lateritic duricrust (cemented ferruginous material), mottled and pallid zones (quartz and clay rich materials), saprolite and saprock (isovolumetrically weathered materials with retention of parent rock fabric), and rock (Anand and Paine 2002).
The end product of latertization is generally pisolitic ferrugenous laterite (Babu and Aseefa 1978).
Dolomite is found as small white rhombohedrons and pisolitic masses.
The Eastport Formation in New Brunswick comprises amygdaloidal mafic flows and agglomerate, massive to flow-banded felsic flows, welded and non-welded lapilli tuff, pisolitic tuff, peperitic breccia, and grey to maroon sandstone and conglomerate totalling ~4000 m (Hay 1967; Pickerill and Pajari 1976; Pickerill et al.
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