1 - HKU Libraries

More documents

Recommendations

Info

Plate 9 - Banded Rhyolite Lava (0895 1364) within the Lantau Formation,Laterally Continuous and Parallel Banding, Nei Lak ShanHighlightingPlate 10 - Complex Ptygmatic Flow Folding in Banded Rhyolitic Lava (0896 1404), within the LantauFormation, Nei Lak Shan
Plate 11 - Pyroclastic Breccia (0869 1399), within the Lantau Formation, North of Nei Lak ShanPlate 12 - Thin Section of Porphyritic Rhyolite Lava (HK9292) (0908 1339), within the LantauFormation, Nei Lak Shan; PPL
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: Plate 7 • Lapilli-Ash Crystal Tuf
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 and 94: Plate 33 - Core stone Development i
Page 95: Plate 37 - Thin Section ofLamprophy
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?