Lee, C.M. (1985). Explanatory notes by C.M.Lee on his stratigraphic column in Table 1. Geological Society ofHong Kong Newsletter, vol.3, no.4, pp 8-9.Lee, C.M., Atherton, M.J., Wu, S., He, G. & Chen, J. (1990). On the geological age of the Repulse Bay Formation,Hong Kong. Report on the Stratigraphy of Hong Kong, Supplement, by MJ. Atherton et al, pp G1-G9.Hong Kong Polytechnic, Department of Civil & Structural Engineering. (Reprinted in Geological Societyof Hong Kong Newsletter, vol. 9, no. 2, 1991, pp 46-51).Le Maitre, R.W. (ed.) (1989). A classification of the igneous rocks and glossary of terms. Recommendations ofthe International Union of Geological Sciences on the systematics of igneous rocks. Blackwell ScientificPublications, Oxford, 193p.Long, K. & Huo, C. (1990). The characteristics of sedimentation in Late Quaternary in Zhujiang (Pearl) RiverDelta. Proceedings of the First International Conference on Asian Marine Geology, Shanghai, edited byWang, P., Lao, Q & He, Q. China Ocean Press, Beijing, pp 213-223.Lumb, P. (1977). The marine soils of Hong Kong and Macau. Proceedings of the International Symposium on SoftClay, Bangkok, pp 45-48. (Published under the title Geotechnical Aspects of Soft Clays, edited by R.P.Brenner & E.W. Brand, Asian Institute of Technology, Bangkok, 1977). (Abstract published inGeotechnical Abstracts, 1979, no. GA 167.04).Nanjing University (1980). Investigation on the time and spatial distribution of the granitic rocks of southeasternChina, their petrographic types and metallogenic relations. Special Publication, Geology Department,Nanjing University, pp 1-56.Nau, P.S. (1979). Geological notes on the sedimentary rocks of Ping Chan Island, Mirs Bay, Hong Kong. Annals ofthe Geographical, Geological & Archaeological Society, University of Hong Kong, no. 7, pp 33-41.Nau, P.S. & Wu, Q.J. (1991). Plant fossils of some sedimentary intercalations within the Repulse Bay volcanicgroup in Hong Kong. Geological Society of Hong Kong Newsletter, vol. 9, no. 2, pp 36-45.Owen, R.B.,Neller,RJ., Shaw, R.& Cheung, P.C.T. (1995). Sedimcntology, geochemistry andmicropalaeontology of Borehole A5/2, West Lamma Channel Hong Kong Geologist, vol. 1, pp 13-25.Peng, C.J. (1978). Hong Kong Minerals. Hong Kong Government Printer, 80 p. (English version and Chineseversion).Peng, C.J. (1983). A Geography of Hong Kong, edited by T.N. Chiu
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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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- Page 124 and 125: Pre-Chek Lap Kok Formation Deposits
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- Page 130 and 131: BOREHOLE NO: A5/1GRID REFERENCE: 80
- Page 132 and 133: formation, thinly laminated clays o
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- Page 136 and 137: Channel and Transgressive Deposits.
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- Page 153 and 154: Non-metalliferous MineralsFissure v
- Page 155 and 156: REFERENCESAddison, R. (1986). Geolo
- Page 157: James, J.W.C. (1993). The offshore
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- Page 167 and 168: Appendix 4aSelective normalized pal
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- Page 171 and 172: construction materials 151contact m
- Page 173 and 174: molybdenite 149Mong Tung Hang 151Mo
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- Page 177: LB 555.125 G34 LGeology of Lantaii