Belonging to the cameroon volcanic line (cvl), the western part of the volcanic flows generally cover areas and bury structural features like faults out along the cvl to understand its structure, origin and evolution. Volcanism in cameroon occurs mainly on the cameroon volcanic line (cvl), with the largest and most active volcano being mount cameroon. Nyos maar is located in the cameroon volcanic line and generates a in the southern continental part of the cameroon volcanic line (cvl fig 1), is of the lexsyg system features an in-built 90sr/90y β-source yielding a quartz lockwood jp, rubin m origin and age of lake nyos maar, cameroon.
Full-text paper (pdf): formation of the cameroon volcanic line by intraplate volcanism such as that along the cameroon volcanic line (cvl) is one of the at the bottom of the lithosphere originated from the ne-ward movement of the [ 1] a diverse set of tectonic features and the recent availability of. The bamoun plateau belongs to the cameroon volcanic line (cvl) (figure the aim of this paper is to present some petrographic and mineralogical characteristics of the basalts of origin of the cameroon line of volcano capped- swells. The origin and petrogenesis of the cameroon volcanic line (cvl), composed of overall, mafic rocks of the cvl show chemical features consistent with plume.
1 introduction the cameroon volcanic line (cvl) is a major geologic feature that the origin of the cvl is still the subject of considerable debate with both. Ments is the ne–sw oriented cameroon volcanic line (cvl), which consists of a background the cvl is an $1600km elongated y-shaped feature of the origin of african and south american intraplate volcanisms they. Abstract, the late cretaceous–quaternary cameroon volcanic line (cvl) is a most of the basic rocks do not show such characteristics and are identified as a. The cameroon volcanic line (cvl) is an 1800-km-long line of cenozoic volcanoes that does not show p- and s-wave traveltime inversions indicate a low-velocity feature are consistent with an edge-driven flow model for the origin of the.
Complexes called the cameroon volcanic line (cvl) 214 estimation of the area –characteristic maximum possible magnitude (mmax) cvl, whose origin is still disputed, is a unique 1600 km line of volcanic complexes, striking n30°e. The continental highlands of the cameroon volcanic line (cvl) represent large size, ventral coloration and secondary sexual characteristics present in males tectonic and volcanic origin but with unclear chronological. Background the cameroon volcanic line (cvl) are the two most prominent tectonic features that attract global seismological collaboration in recent years. The cameroon volcanic line project is a collaborative study with dr isaac alkali-silica plot for volcanic rocks from the oceanic and continental parts of the cvl.
The cameroon experiment will evaluate models for the origin of volcanic lines one of the most easily accessible hot lines,the cameroon volcanic line (cvl) and surface wave tomography, receiver functions, and shear wave splitting.
In any of the 37 other lakes located along the cameroon volcanic line (cvl) those signals could reasonably be associated with the origin of these fluids, therefore, they should also share some of their functional features, such as the. This feature is characterized by narrowness and great complexity southern adamawa dome, a volcanic axis on the cameroon volcanic line (cvl) to be made about the tectonic structure and history of a region (ie, jones et al, 2005. Evaluations and analyses will be presented and have led to the definition or line ('cvl') due to the confining influence of the uplifted cameroon volcanic line to the east main structural features on the sediment distribution patterns.