Xu, X., O’reilly, S.Y., Griffin, W.L., Zhou, X.M. and Huang, X.L. (1998) The Nature of the Cenozoic Lithosphere at Nushan, Eastern China. In: Flower, M.F.J., Ed., Mantle Dynamics and Plate Interactions in East Asia, American Geophysical Union, Washington DC, 167-195.
http://dx.doi.org/10.1029/GD027p0167

has been cited by the following article:

• TITLE: Spinel-Bearing Lherzolite Xenoliths from Hosséré Garba (Likok, Adamawa-Cameroon): Mineral Compositions and Geothermobarometric Implications

  AUTHORS: Nguihdama Dagwai, Chazot Gilles, Kamgang Pierre, Mbowou Gbambié Isaac Bertrand, Ngounouno Ismaïla

  KEYWORDS: Xenoliths, lherzolite, Geothermobarometry, Likok, Adamawa

  JOURNAL NAME: International Journal of Geosciences, Vol.5 No.12, November 18, 2014

  ABSTRACT: Spinel-bearing lherzolite xenoliths from the Hossere Garba (1272 m.a.s.l) volcano on the Adamawa Plateau, is located in Likok village, at about 35 km to WSW of Ngaoundere. These xenoliths (~11 cm size) have been sampled into the host basaltic lava flows from the NE flank of the Hossere Garba volcano. These xenoliths characterized by porphyroclastic texture consisted of olivine (~55 vol.%), orthopyroxene (~19 vol.%) and clinopyroxene (~21 vol.%) crystals. Spinel crystals (~5 vol.%) are red brown and interstitial between the crystals of olivine and pyroxenes. CaO contents are low (VI/AlIV ratio range between 1.1 and 1.3 for the Cr-diopside crystals from Hossere Garba xenoliths. The constant value of the volumes V(Cell) and V(M1) for clinopyroxene compositions, indicates the similar pressures. Hossere Garba represents a residual sequence issued from partial melting of a mantle source. Similar compositions have been recorded in minerals of ultramafic xenoliths from other ultramafic xenoliths domains of the Cameroon Line and the Adamawa Plateau.