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Appendix 2 (continued)Sample HK5570 HK9988 HK8555 HK9767HK9841HK9855Si02Ti02A1203Fe203*MnOMgOCaONa2OK2OP2O5Total75.570.1012.571.430.030.200.873.165.090.0299.0476.790.0712.131.750.10-0.163.884.820.0199.7168.320.4714.254.960.090.561.873.195.300.1499.1575.120.1812.841.830.020.160.393.245.830.0399.6477.810.0512.520.260.123.265.1399.1551.571.3616.499.950.144.298.302.671.740.4196.92LOI 1.030.301.220.450.832,77CrNiCoScVCuPbZn6-2-3-3121151081133771049711372329124371282161132127321925192181480SnWMo16-55322429112SAs--RbBaSrGa30317552183412314201554200122183158035482274472532NbZrTiYThU201496004939743171420744711189281834254161831079383446711130083478914081533032LaCe316230656312063127471856HK5570HK9988HK8555HK9767HK9841HK9855Fine-grained granite, Tsing Nam WanPorphyritic fine-grained syenite, long Fuk Mui WanFeldsparphyric rhyolite, Discovery BayPorphyritic microgranite, Pa Tau KwuQuartzphyric rhyolite, Penny's BayBasalt, SamPak2795521330101650973020125 1733023425 20060215752043519160 19655162
Appendix 2 (continued)Sample HK10547Si02Ti02A12O3Fe203*MnOMgOCaONa2OK2OP205Total54.651.4814.7610.570.193.917.200.933.440.2997.42LOI 1.82HK973974.190.1813.881.880.020.190.242.146.170.0498.931.06CrNiCoScVCuPbZnSnWMoSAsRbBaSrGaNbZrTiYThULaCe261426-- 821211_11«.5074093882017178887335333082473,92342928---3651024167-14209107937«856129HK10547HK9739Lamprophyre, Tsing YiAplite, YiChuen26575 238302376022315163
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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
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Chapter 9Superficial GeologyIntrodu
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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 and 160: Sewell, R.J., Strange, PJ., Langfor
Page 161 and 162: Appendix 1Microfossils identified f
Page 163: Appendix 2 (continued)Sample HK9913
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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