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James, J.W.C. (1993). The offshore geology of the area around Lantau Island, Hong Kong. British GeologicalSurvey, Keyworth, U.K., 74 p. (Technical Report, WB/93/13R).Jolley, D.W. (1992a). Palynological Analysis of Samples from the Huang Jau t Sham Wat and Chek Lap KokFormations (Quaternary) of Borehole A5/1, Soko Islands, Hong Kong. British Geological Survey,Keyworth, U.K., 10 p. (Technical Report, Stratigraphy Series, WH/92/241).Jolley, D. W. (1992b). A Palynological Report on the Interval 0.1 m~ 32.5m in the Offshore Hong Kong BoreholeESC 17. British Geological Survey, Keyworth, U.K., 11 p. (Technical Report, Stratigraphy SeriesWH/92/211C).Jones, W.A. (1927). The Petrography of the Rocks of Hong Kong. MASc Thesis, University of British Columbia,82 p. plus 1 map.Judd, A.G. (1989). Shallow Gas Group Newsletter, no.l, 1 p.Kemp, SJ. (1993). Mineralogical and Particle-size Analyses of Quaternary Sediments from Offshore BoreholeESC 17, Hong Kong. British Geological Survey, Keyworth, U.K., 14 p. (Technical Report, WG/93/8C).Kendall, F.H. (1976). High Island: A study of undersea deposits. Journal of the Hong Kong ArchaeologicalSociety, vol. 6, pp 26-32.Koutsoftas, D.C., Foott, R. & Handfelt, L.D. (1987). Geotechnical investigations offshore Hong Kong. Journal ofGeotechnical Engineering, American Society of Civil Engineers, vol. 113, pp 87-105. (Discussion, vol.114, 1988, pp 1059-1061). (Abstract published inASCE Transactions, vol. 152, 1987, pp 140, and inGeotechnical Abstracts, 1987, no. GA 321.80).Lai, K.W. (1977). Major geotectonic features of Hong Kong. Hong Kong Baptist College Academic Journal, vol. 1,no. 4, pp 241-286. (In Chinese with English abstract).Lai, K.W. (1982). Discussion on the colluvium of Hong Kong (8th October 1980). Hong Kong Baptist CollegeAcademic Journal, vol. 9, pp 139-158.Lai, K.W. (1993). Major fault zones in Shenzhen and nearby areas. Geological Society of Hong Kong Newsletter,vol.11, no.1-2, pp2-7.Lai, K.W. &. Langford, R.L. (1991). Spatial and temporal characteristics of major faults of Hong Kong.Proceedings of the International Conference on Seismicity in Eastern Asia, Hong Kong, in press. (Abstractpublished in Geological Society of Hong Kong, Abstracts no. 7, 1991, pp 21-22).Lai, K.W. & Mui, M, (1984). The stratigraphy of the Lok Ma Chau Formation in Hong Kong. Hong Kong BaptistCollege Academic Journal, vol. 11, pp 177-185.Lai, K.W. & Mui, M. (1985). Lithostratigraphic comparison of the Lok Ma Chau Formations of Hong Kong withCarboniferous Strata of Shenzen and Guangzhou. Geological Society of Hong Kong Newsletter, vol. 3, no.2, pp 4-7,Lai, K.W. & Taylor, B,W. (1983). The classification of colluvium in Hong Kong. Proceedings of the Meeting onGeology ofSurficial Deposits in Hong Kong, Hong Kong, pp 75-85. (Published as Geological Society ofHong Kong Bulletin no. 1, edited by W.W.S. Yim, 1984). (Abstract published in Geological Society ofHong Kong, Abstracts no. 1,1983, pp 23).Langford, R.L. (1990). Geology of Chek Lap Kok, Geological Society of Hong Kong Newsletter, vol. 8, part 4, pp21-39.Langford, R.L, (1994), Geology of Chek Lap Kok Geotechnical Engineering Office, Hong Kong, 61 p. (HongKong Geological Survey Sheet Report No. 2).Langford, R.L & Adlam, KA McL. (1985). Vector: A Computer Program for the Analysis and Manipulation ofThree-Dimensional Orientation Data. Engineering Development Department, Hong Kong, 27p.Langford, R.L, Lai, K.W., Arthurton, R.S. & Shaw, R. (1989). Geology of the Western New Territories.Geotechnical Control Office, Hong Kong, 140 p. (Hong Kong Geological Survey Memoir No. 3).155
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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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- 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 155: REFERENCESAddison, R. (1986). Geolo
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- Page 161 and 162: Appendix 1Microfossils identified f
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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