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Hong Kong Geology Guide Book Geotechnical Engineering Office ...

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In addition to extensive exposures in the northern New Territories, the Carboniferous<br />

sedimentary rocks of the San Tin Group are also present below Yuen Long and Tin<br />

Shui Wai, and along the eastern side of the Tuen Mun Valley. The San Tin Group<br />

carbonate rocks occur offshore on the northern side of Lantau Island. There, they are<br />

entirely covered by Quaternary superficial deposits, having been proven by drillholes.<br />

The carbonate rocks (now metamorphosed to marble) of the Yuen Long Formation are<br />

soluble, resulting in the formation of solution cavities that have had important<br />

consequences for designing and constructing building foundations in the area.<br />

The graphite bearing siltstone and graphitic schist exposed on The Brothers islands to<br />

the north of Lantau Island belong to the Mai Po Member of the Lok Ma Chau<br />

Formation. Detailed studies have concluded that the Lok Ma Chau Formation was<br />

deposited in a prograding delta (Lai et al., 1988). A prograding delta is one that<br />

extends progressively seaward from a river mouth. Sandstone, conglomeratic<br />

sandstone, and conglomerate are typical deltaic sediments. In contrast, evidence<br />

suggests that the fine sandstone, siltstone and carbonaceous layers of the Mai Po<br />

Member were deposited in a near-shore tidal flat or on the alluvial plain of a delta.<br />

References<br />

Allen, P. M. & Stephens, E. A. 1969. Interim report on the Geological Survey of <strong>Hong</strong><br />

<strong>Kong</strong>. Overseas Division, Institute of Geological Sciences, London, 133 p.<br />

Allen, P. M. & Stephens, E. A. 1971. Report on the Geological Survey of <strong>Hong</strong> <strong>Kong</strong>.<br />

Government Printer, 107 p. plus 2 maps.<br />

Atherton, M.J. & Burnett, A.D. 1986. <strong>Hong</strong> <strong>Kong</strong> Rocks. Published by the Urban<br />

Council, <strong>Hong</strong> <strong>Kong</strong>, 145 p.<br />

Bennett, J.D. 1984b. Review of <strong>Hong</strong> <strong>Kong</strong> Stratigraphy. GCO Publication No. 5/84,<br />

<strong>Geotechnical</strong> Control <strong>Office</strong>, <strong>Hong</strong> <strong>Kong</strong>, 62 p.<br />

Chan, M.C. 1987. Petrography of the Lower Carboniferous San Tin Group, <strong>Hong</strong> <strong>Kong</strong>.<br />

Geological Society of <strong>Hong</strong> <strong>Kong</strong> Newsletter, v. 5, no. 2, pp 9 - 15.<br />

Davis, S.G. 1952. The geology of <strong>Hong</strong> <strong>Kong</strong>. Government Printer, <strong>Hong</strong> <strong>Kong</strong>. 231 p.<br />

plus 14 plates & 3 maps.<br />

Fletcher, C.J.N., Campbell, S.D.G., Busby, J.P., Carruthers, R.M. & Lai, K.W. 1997.<br />

Regional tectonic setting of <strong>Hong</strong> <strong>Kong</strong>: implications of new gravity models.<br />

Journal of the Geological Society, v. 154, pp 1021–1030.<br />

Frost, D.V. 1992. <strong>Geology</strong> of Yuen Long, <strong>Hong</strong> <strong>Kong</strong> Geological Survey Sheet Report<br />

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