<?xml version="1.0" encoding="UTF-8"?>
<records>
<record>
<language>eng</language>
<publisher>Science and Education Publishing</publisher>
<journalTitle>Journal of Geosciences and Geomatics</journalTitle>
<eissn>2373-6704</eissn>
<publicationDate>2021-06-14</publicationDate>
<volume>9</volume>
<issue>2</issue>
<startPage>66</startPage>
<endPage>73</endPage>
<doi>10.12691/jgg-9-2-3</doi>
<publisherRecordId>JGG2021923</publisherRecordId>
<documentType>article</documentType>
<title language="eng">Petrological Characterization of Pelites from the Mintom Basin and Their Weathering Mantle</title>
<authors>
<author>
<name>Ondoua Oyono Joseph Sadrac</name>
<email>ondoua171@yahoo.fr</email>
<affiliationId>1</affiliationId>
<affiliationId>2</affiliationId>
</author>
<author>
<name>Ekomane Emile</name>
<affiliationId>2</affiliationId>
</author>
<author>
<name>Ipan Antoinette Solange</name>
<affiliationId>2</affiliationId>
<affiliationId>3</affiliationId>
</author>
<author>
<name>Edima Yana Roland William</name>
<affiliationId>3</affiliationId>
<affiliationId>4</affiliationId>
</author>
<author>
<name>Bidjo Emvoutou G¨¦ry Christian</name>
<affiliationId>4</affiliationId>
<affiliationId>4</affiliationId>
</author>
<author>
<name>Bitom Dieudonn¨¦</name>
<affiliationId>4</affiliationId>
</author>

</authors>
<affiliationsList>
<affiliationName affiliationId="1">Institute of Agricultural Research for Development, P.O.Box:2067, Yaound¨¦, Cameroon</affiliationName>





</affiliationsList>
<abstract language="eng">The aim of the present study is to characterize a weathering mantle developed on pelitic rock in the tropical forest region precisely in Mintom (South East Cameroun). This characterization include morphology, physico-chemical and mineralogic analyses. The region is characterize by a hot and wet climate consisting of four seasons of inequal length and intensity. The average temperature is about 24&#176;C and the mean rainfall is about 1633mm/years. The rocks in the area consist of limestone, dolomites and pelites. Fieldwork consist of landscape analysis, geologic prospection and soil profile description. Mineralogical and physico-chemical was carried out on various samples in the laboratory. Morphological results show that the studied profile has a general brownish yellow aspect, with a thickness of about 6m and a silty-clayey texture. Five horizons can be distinguished from top to bottom: a humiferous horizon, a loose yellow set, a yellow horizon bearing quartz fragments and large indurated blocks, a saprolite consisting of a fine and coarse saprolite possessing some pelite relics of variable sizes and a deep red colour just like that of the parent rock. The parent rock is a massive pelite with a reddish colour when wet and a violet colour when dry. It has a powdery feel. Analytically, the soils have an acidic pH (4,0 to 4,2), a high organic matter content (4,8%), a C/N ratio of about 6,76, a cationic exchange capacity of 7,64meq/100g with a saturation rate S/T of about 7. Particle size distribution shows that the silty fraction is dominant (59%), followed by the clayey fraction (30%). The main minerals are kaolinite, quartz, smectites, calcites, dolomites, goethite and hematite.</abstract>
<fullTextUrl format="pdf">http://pubs.sciepub.com/jgg/9/2/3/jgg-9-2-3.pdf</fullTextUrl>
<keywords language="eng"><keyword>pelitic rocks</keyword>
<keyword>weathering mantle</keyword>
<keyword>petrology</keyword>
<keyword>Zoebefam</keyword>
<keyword>Mintom</keyword>
<keyword>South East Cameroon</keyword>
</keywords>
</record>
</records>
