... as a fault-bounded block exposed on the eastern end of the Aileu Complex ( Fig. 1 B; Berry 1981 ), is at least partly responsible for the steep gravity anomaly on the north coast. According to Berry (1981) , the most common rock-type present within the Hili Manu peridotite is a fine-grained, pale brown...

.... The proportion of mafic rocks increases toward the east, where the Aileu Complex is bounded by the Hili Manu amphibolite and ultramafic massifs. Berry & McDougall (1986) considered this amphibolite body to be part of the Aileu Complex, whereas Charlton (2002) suggested that it is part of the Hili Manu...

... ), there is a distinct increase in metamorphic gradient northeastward through a parautochthonous sedimentary-volcanic succession toward the Hili Manu lherzolite, located at the eastern end of the metamorphic complex ( Berry, 1981 ; Berry and Grady, 1981 ). Hamilton (1979) and Charlton (2002c) have interpreted...

...: Refinement of Multi-Scale Data and Integration in Numerical Modelling: Geological Society, London, Special Publication 322 , p. 99 – 114 . Berry R.F. , 1981 , Petrology of the Hili-Manu Lherzolite, East Timor : Journal of the Geological Society of Australia , v. 28 , no. 3–4 , p. 453 – 469...

... Phreatomagmatic boulder conglomerates at the tip of the ca 2772 Ma Black range dolerite dyke, Pilbara Craton, Western Australia— M.J. Van Kranendonk, W. Bleeker, and J. Ketchum 617 Whole-rock geochemistry of the Hili Manu peridotite, East Timor: Implications for the origin of Timor ophiolites— T.J. Falloon...