1 - HKU Libraries

More documents

Recommendations

Info

Plate 35 - Lamprophyre Dyke TrendingEast, Intruding MegacrysticFine-grained Granite (12031964), Fui Yiu WanPlate 36 - Thin Section of Very Fine-grained Basalt (HK 10684) (1152 1810), from Chek Lap Kok; XPL
Plate 37 - Thin Section ofLamprophyre (HK10859) (1117 1986), Chek Lap Kok; XPL plus ; /A plate\ cPlate 38 -Aplite Dyke in Medium-grained Granite (2070 0902), Cheung Chau
Page 2 and 3:
UNIVERSITY OF HONG KONGLIBRARIES
Page 4 and 5:
© Government of Hong KongPublished
Page 7 and 8:
CONTENTSTitle pagePage1ForewordCont
Page 9 and 10:
Distribution and Lithology 73Detail
Page 11 and 12:
Chapter 10 Economic Geology 149Intr
Page 13 and 14:
(Plates)Plate 22 - Porphyritic Medi
Page 15:
Table 1 — Grain Size Description
Page 18 and 19:
0 1 2 3 4 5 k mCONTOURS AT 100m INT
Page 20 and 21:
properties of the marine deposits b
Page 22 and 23:
Archival DataAll records from the s
Page 24 and 25:
Chapter 2Outline of GeologyThe soli
Page 26 and 27:
The Mesozoic volcanic rocks are div
Page 29 and 30:
Chapter 3Palaeozoic Sedimentary Roc
Page 31 and 32:
Carboniferous metasedimentaiy rocks
Page 33 and 34:
Plate 1 - Fining-Upward Sequence of
Page 35 and 36:
Plate 3 - Well-bedded Sandstones an
Page 37 and 38:
Reef Island. The northern end of th
Page 39 and 40:
Table 3. Evolution of Nomenclature
Page 41 and 42:
are crudely stratified and welded i
Page 43 and 44: Shing Mun FormationThe type localit
Page 45 and 46: Tai Che Tung. Crystal tuff, interpr
Page 47 and 48: Plate 7 • Lapilli-Ash Crystal Tuf
Page 49 and 50: Plate 11 - Pyroclastic Breccia (086
Page 51 and 52: appears fragmental, and contains mu
Page 53 and 54: exposures in the stream bed consist
Page 55 and 56: Lin Fa Shan. The steep eastern flan
Page 57 and 58: dipping northwest at 46°, is prese
Page 59 and 60: Sunset Peak MemberThe Sunset Peak M
Page 61 and 62: Plate 16- Block and Lapilli-bearing
Page 63 and 64: Chapter 5Major IntrusionsClassifica
Page 65 and 66: in grain size from 0.4 to 1.5 mm, a
Page 67 and 68: 20 - Megacrystic Medium-grained Gra
Page 69 and 70: Pui O Wan. Porphyritic medium-grain
Page 71 and 72: minimum age of c. 145 Ma (see earli
Page 73 and 74: The granite on Chek Lap Kok is most
Page 75 and 76: Southeast of Tin Sam, on the wester
Page 77 and 78: About 1 km east of Nam Shan, exposu
Page 79 and 80: Plate 25 - Thin Section of Porphyri
Page 81 and 82: Chapter 6Minor IntrusionsIntroducti
Page 83 and 84: The microgranite grades southwards
Page 85 and 86: the Lantau Formation, however, and
Page 87 and 88: Plate 29 - Flow-banded Quartzphyric
Page 89 and 90: also cut volcanic rocks of the Tsue
Page 91 and 92: Silver Mine Bay. On the headland so
Page 93: Plate 33 - Core stone Development i
Page 98 and 99: Pre-Yensfaanlan StructureWithin the
Page 100 and 101: separates areas of different lithol
Page 102 and 103: NeotectonicsFault activity in the r
Page 105 and 106: Chapter 8Metamorphism and Alteratio
Page 107 and 108: 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 and 160:
Sewell, R.J., Strange, PJ., Langfor
Page 161 and 162:
Appendix 1Microfossils identified f
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
show all

1 - HKU Libraries

Create successful ePaper yourself

Delete template?

Save as template?