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This monograph conducts a syntactic study of Tuki, a Bantu language spoken in Cameroon, from a cartographic perspective. The following domains are meticulously explored: The Complementizer Domain, the Inflectional Domain and the Verbal Domain. This study reveals that there is a relative phrase (RelP) located between ForceP and FocP. Moreover, a detailed analysis of an articulated IP provides the order of clausal functional heads that manifest aspectual morphology, which is theoretically closely related to issues in adverbial syntax. Additionally, the language under study unveils a very rich
Tuki language --- Bacenga language --- Baki language (Cameroon) --- Batchenga language --- Betsinga language --- Betzinga language --- Ki language --- Oki language (Cameroon) --- Osa Nanga language --- Sanaga language (Tuki) --- Bantu languages --- Syntax. --- Grammar.
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The principal aim of this book is to provide a wide range of information and a useful reference for researchers interested to investigate heavy mineral assemblages in different geological settings and for a variety of purposes. The methodological developments achieved in recent years for the identification of heavy minerals in a wide grain-size range are illustrated. All factors that affect heavy mineral concentration and relative proportions, including hydraulic sorting, mechanical abrasion, chemical weathering, and post-depositional dissolution, and all factors able to introduce analytical, environmental, or diagenetic bias are thoroughly addressed. A proper integration of multiple techniques including bulk sediment, multi-mineral, and single-mineral methods are discussed by renowned authors in their invited contributions.
heavy minerals --- correlation --- North Sea --- Jurassic --- Triassic --- Carboniferous --- Devonian --- relative and absolute abundances --- sampling strategy --- size-window for analysis --- heavy mineral point-counting --- provenance and plate-tectonic setting --- chemical weathering --- hydraulic sorting --- recycling --- diagenesis --- sediment --- provenance --- statistics --- zircon --- point counting --- petrography --- mineral grains composition --- surface textures --- sources --- WNW Portuguese Continental Margin --- Raman spectroscopy --- sedimentary provenance --- automatization --- heavy mineral --- Pliocene --- the Changjiang Delta --- amphibole --- surface texture --- garnet --- epidote --- pyroxene --- provenance tracers --- varietal studies --- mineral chemistry --- semi-automated Raman counting --- Ladakh-Kohistan arcs --- Himalaya --- Nanga Parbat --- Karakorum --- Indus river --- amphiboles --- tremolite --- actinolite --- provenance analysis --- tectonic versus climatic control --- early-middle Pleistocene transition --- Yellow River terraces --- Lanzhou (northern China) --- sieving of fine silt --- fallacy of laser granulometry --- benthic foraminifera --- Ganga–Brahmaputra river system --- Bay of Bengal --- Himalayan orogen --- bulk-sediment petrography --- bulk-sediment geochemistry --- selective entrainment --- suspension sorting --- chemical indices of weathering --- sediment budgets --- Brahmaputra River --- Ganga River --- handbook for laboratory procedures --- nontoxic heavy liquids --- wet sieving of silt --- zircon separation --- heavy-mineral mounts --- n/a --- Ganga-Brahmaputra river system
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