@article{fdi:23236,
  title = {{C}rustal structure of the {A}damawa {P}lateau {C}ameroon},
  author = {{S}tuart, {G}.{W}. and {F}airhead, {J}.{D}. and {D}orbath, {L}ouis and {D}orbath, {C}atherine},
  editor = {},
  language = {{ENG}},
  abstract = {{R}ecordings of quarry blasts along a 300 km profile across the {A}damawa {P}lateau at the eastern of the {C}ameroon {V}olcanic {L}ine permitted the determination of the crustal structure of the region. {T}o the north of the {P}lateau the crust is about 23 km thick. {T}he southern part of the {P}lateau by comparison is associated with a more normal crustal thickness of about 33 km. {B}etween these two areas the seismological experiment was not able to delineate how the croust changes. {H}owerer, if the topography and gravity field reflect crustal thickness then there is a rapid change in crustal thickness at the northern edge of {A}damawa {P}lateau.},
  keywords = {{CROUTE} {CONTINENTALE} ; {MANTEAU} ; {DISCONTINUITE} {DE} {MOHOROVICIC} ; {ANOMALIE} {DE} {BOUGUER} ; {SISMOGRAMME} ; {CAMEROUN} ; {CAMEROUN} {CENTRE} ; {ADAMAOUA} {PLATEAU}},
  booktitle = {},
  journal = {{R}evue {S}cience et {T}echnique.{S}{\'e}rie {S}ciences de la {T}erre},
  volume = {1},
  numero = {1/2},
  pages = {25--35},
  ISSN = {0258-4840},
  year = {1985},
  URL = {https://www.documentation.ird.fr/hor/fdi:23236},
}