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Whiteside, P.G.D. & Wragge-Morley, N. (Editors) (1988). Marine Sand and Gravel Resources of Hong Kong.(Proceedings of the Seminar on Marine Sources of Sand, Hong Kong, December 1987). Geological Societyof Hong Kong, 221 p.Whyte, R.O. (Editor) (1984). The Evolution of the East Asian Environment (Proceedings of the Conference on thePalaeoenvironment of East Asia from the Mid-Tertiary, Hong Kong, January 1983). Centre of AsianStudies, Hong Kong University, 2 volumes, 982 p. (Occasional Papers and Monographs, no.59).Whyte, P., Aigner, IS., Jablonski, N.G., Taylor, G., Walker, D., Wang, P.X. and So, C.L. (1988). The Evolution ofthe East Asian Environment. (Proceedings of the Second Conference on the Palaeoenvironment of EastAsia from the Mid-Tertiary, Hong Kong, January 1987). Centre of Asian Studies, University of Hong Kong,2 volumes, 1219 p. (Occasional Papers and Monographs, no.77).Wilkinson, IP. (1990). Calcareous Microfossils from the Quaternary of Chek Lap Kok Airport Borehole B15,Hong Kong. British Geological Survey, Keyworth, U.K., 6 p. (Technical Report, Stratigraphy Series,WH/90/175).Wilkinson, IP. (1991). Quaternary Foraminifera from Hong Kong, Borehole Number A5/L British GeologicalSurvey, Keyworth, U.K., 3 p. (Technical Report, Stratigraphy Series, WH/91/263C).Wilkinson, IP. (1992a). Calcareous microfaunas from Chek Lap Kok Borehole ESC 17 (Hong Kong). BritishGeological Survey, Keyworth, U.K., 8 p. (Technical Report, Stratigraphy Series, WA/92/163C).Wilkinson, IP. (1992b). Foraminifera from the Late Quaternary and Holocene of Borehole A5/1 (Hong Kong).British Geological Survey, Keyworth, U.K., 2 p. (Technical Report, Stratigraphy Series, WA/92/169C).Williams, M.Y. (1943). The stratigraphy and palaeontology of Hong Kong and the New Territories. Transactionsof the Royal Society of Canada, third series, vol. 37, sect. IV, pp 93-117.Williams, M.Y., Brock, R.W., Schofield, SJ. & Phemister, T.C. (1945). The physiography and igneous geology ofHong Kong and the New Territories. Transactions of the Royal Society of Canada* third series, vol. 39,sect. V,pp 91-119.Woods, N.W. & Langford, R.L. (1991). The geology and exploitation of the West Brother Island graphite deposit.Geological Society of Hong Kong Newsletter, vol. 9, no, 2, pp 24-35.Woodcock, N.H. and Naylor, M. (1983). Randomness testing in three-dimensional orientation data. Journal ofStructural Geology, vol.5, no.5, pp 539-548.Yim, W.W.S. (1984a). Evidence for Quaternary environmental changes from sea-floor sediments in Hong Kong, In:Whyte, R.O.77i
Appendix 1Microfossils identified from samples of the Carboniferous Mai Po Member by ChinaCorelab (CC), Shekou, Shenzhen, and Guangdong Institute of Geological Sciences (GIGS)HK 7250,14600 21150, West Brother Island (CC)Calamospora breviradiataCalamospora sp.Densosporites annulatusTriquitrites trivalvisLaevigatosporites sp.Leiotriletes sp.HK 9284, 02765 13075, Tai O, Lantau Island (GIGS)Gorgonisphaehdium ? sp.Knoxisporites litheratus (Waltz) PlayfordKnoxisporites sp.Laevigatosporites sp.Lycospora sp.Lycospora pusilla (Ibrahim)The organic residue recovered from this sample contained a few miospores. Knoxisporiteslitheratus, Lycospora pusilla and Gorgonisphaeridium sp. indicate a Carboniferous age inSouth China.HK 8433,13245 13350, Sunset Peak (GIGS)In No. 8433 some badly preserved inside cores were found and identified as Bairdia sp.,Cytherellina sp., Amphissites sp. and Parapachites sp. The latter three genera may be LatePalaeozoic in age.Age: ?Late Palaeozoic159
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UNIVERSITY OF HONG KONGLIBRARIES
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© Government of Hong KongPublished
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CONTENTSTitle pagePage1ForewordCont
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Distribution and Lithology 73Detail
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Chapter 10 Economic Geology 149Intr
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(Plates)Plate 22 - Porphyritic Medi
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Table 1 — Grain Size Description
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0 1 2 3 4 5 k mCONTOURS AT 100m INT
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properties of the marine deposits b
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Archival DataAll records from the s
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Chapter 2Outline of GeologyThe soli
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The Mesozoic volcanic rocks are div
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Chapter 3Palaeozoic Sedimentary Roc
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Carboniferous metasedimentaiy rocks
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Plate 1 - Fining-Upward Sequence of
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Plate 3 - Well-bedded Sandstones an
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Reef Island. The northern end of th
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Table 3. Evolution of Nomenclature
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are crudely stratified and welded i
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Shing Mun FormationThe type localit
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Tai Che Tung. Crystal tuff, interpr
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Plate 7 • Lapilli-Ash Crystal Tuf
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Plate 11 - Pyroclastic Breccia (086
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appears fragmental, and contains mu
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exposures in the stream bed consist
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Lin Fa Shan. The steep eastern flan
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dipping northwest at 46°, is prese
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Sunset Peak MemberThe Sunset Peak M
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Plate 16- Block and Lapilli-bearing
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Chapter 5Major IntrusionsClassifica
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in grain size from 0.4 to 1.5 mm, a
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20 - Megacrystic Medium-grained Gra
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Pui O Wan. Porphyritic medium-grain
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minimum age of c. 145 Ma (see earli
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The granite on Chek Lap Kok is most
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Southeast of Tin Sam, on the wester
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About 1 km east of Nam Shan, exposu
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Plate 25 - Thin Section of Porphyri
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Chapter 6Minor IntrusionsIntroducti
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The microgranite grades southwards
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the Lantau Formation, however, and
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Plate 29 - Flow-banded Quartzphyric
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also cut volcanic rocks of the Tsue
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Silver Mine Bay. On the headland so
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Plate 33 - Core stone Development i
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Plate 37 - Thin Section ofLamprophy
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Pre-Yensfaanlan StructureWithin the
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separates areas of different lithol
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NeotectonicsFault activity in the r
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Chapter 8Metamorphism and Alteratio
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the majority of rocks in the distri
Page 109: Chapter 9Superficial GeologyIntrodu
Page 112 and 113: Detailstal O. Alluvial deposits for
Page 114 and 115: trains. The regolith on most steep
Page 116 and 117: Plate 44 - Boulder Debris on the So
Page 118 and 119: gazetted for recreational purposes.
Page 120 and 121: DetailsTai O. Extensive intertidal
Page 122 and 123: Plate 48 - Sandy Beach at Fan Lau S
Page 124 and 125: Pre-Chek Lap Kok Formation Deposits
Page 126 and 127: formation. The sequence is usually
Page 128 and 129: BOREHOLE NO: ESC 17GRID REFERENCE:
Page 130 and 131: BOREHOLE NO: A5/1GRID REFERENCE: 80
Page 132 and 133: formation, thinly laminated clays o
Page 134 and 135: Quinqueloculina seminulum, which is
Page 136 and 137: Channel and Transgressive Deposits.
Page 138 and 139: Figure 20 - Areas of Acoustic Turbi
Page 140 and 141: West Lamma Channel These may be att
Page 142 and 143: Figure 23 - Depth-Averaged, Maximum
Page 144 and 145: The formation is Holocene in age. T
Page 146 and 147: Boreholes (A5/1, A5/2, B2/1, ESC17
Page 148 and 149: Plate 51 - Deep Weathering Profile
Page 151 and 152: Chapter 10Economic GeologyIntroduct
Page 153 and 154: Non-metalliferous MineralsFissure v
Page 155 and 156: REFERENCESAddison, R. (1986). Geolo
Page 157 and 158: James, J.W.C. (1993). The offshore
Page 159: Sewell, R.J., Strange, PJ., Langfor
Page 163 and 164: Appendix 2 (continued)Sample HK9913
Page 165 and 166: Appendix 2 (continued)Sample HK1054
Page 167 and 168: Appendix 4aSelective normalized pal
Page 169 and 170: ,Appendix 5 -Radiocarbon and Other
Page 171 and 172: construction materials 151contact m
Page 173 and 174: molybdenite 149Mong Tung Hang 151Mo
Page 175 and 176: talus 107,115Tarn Tsui Wan 71,87Tan
Page 177: LB 555.125 G34 LGeology of Lantaii
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