- Page 2 and 3: UNIVERSITY OF HONG KONGLIBRARIES
- Page 4 and 5: © Government of Hong KongPublished
- Page 8 and 9: Repulse Bay Volcanic Group 43Lantau
- Page 10 and 11: Hydrothermal Alteration 103Kaoliniz
- Page 12 and 13: (Figures)15 Geological Log of Boreh
- Page 14 and 15: and* This memoir describes the geol
- Page 17 and 18: Chapter 1IntroductionLocation and P
- Page 19 and 20: of the district. Ma Wan near Tsing
- Page 21 and 22: Present SurveyGeological field mapp
- Page 23 and 24: Figure 4 - Location of Boreholes an
- Page 25 and 26: Table 2-SoIid Rocks and Superficial
- Page 27: alteration of volcanic and adjacent
- Page 30 and 31: The thickness of the marble is poor
- Page 32 and 33: fine-grained sandstone and siltston
- Page 34 and 35: The contact between foliated sandst
- Page 36 and 37: Plate 5 - Near Vertical Quartzitic
- Page 38 and 39: Chapter 4Mesozoic Volcanic and Sedi
- Page 40 and 41: Pumice, glassCrystals,crystalfragme
- Page 42 and 43: contain porph>Titic lapilii t>pical
- Page 44 and 45: ashes, in contrast with the coarser
- Page 46 and 47: These beds are extensive in the wes
- Page 48 and 49: Plate 9 - Banded Rhyolite Lava (089
- Page 50 and 51: Plate 13 - Thin Section of Spheruli
- Page 52 and 53: Volcanic EnvironmentEuhedral crysta
- Page 54 and 55: and 500 m to the east (1434 1246) a
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Two samples from Lantau Peak, analy
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Details J .Pak Kok. On the east sid
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abundant very fine-grained lithic f
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Plate 18 - Thin Section ofGranodior
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GranodioriteDistribution and Lithol
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against the granite country rock. M
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Plate 22 - Porphyritic Medium-grain
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Hei Ling Chan. Porphyritic medium-g
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fresh is pleochroic, varying from l
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200 m to the south, there is a irre
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Quartz syenite is poorly exposed in
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Exposures of the eastern outcrop of
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3j A 4: 5 6' 7 8 9 l o--*'»•"»'
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Feldsparphyric rhyolites and porphy
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idge of Tsing Yi. The dykes, expose
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Peng Chau. On the northern coast of
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Plate 31 - Thin Section ofMegacryst
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Lam Chau. An altered basalt dyke cr
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A typical, finer-grained sample of
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Plate 35 - Lamprophyre Dyke Trendin
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Chapter 7StructureIntroductionThe s
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The Lantau CalderaThe clearest stru
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The northeast- and northwest-trendi
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Plate 39 - Foliated Basalt Dyke Cut
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ocks adjacent to the caldera margin
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maps as metasandstones and metasilt
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Rock andweathered rockFigure 12 - S
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Mui Wo. Extensive alluvial flats oc
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Plate 42 - Fluvial and Slope Deposi
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Yam O Wan - Yi Fak Wan. Small, isol
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Sz Pak Wan - Sam Pak Wan - Yi Pak W
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Plate 46 - Raised Sand Bar or Dune
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of uncertain stratigraphical signif
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Urmston Road - Brothers proto - cha
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filling channels and transporting s
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Sham Wat FormationThe Sham Wat Form
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Approximate depth (metres)Two-way t
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BOREHOLEBENTHONIC FORAMINIFER1DAPLA
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811 490E820 520NPD-iUrmston Road -
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Figure 19 - Distribution and Thickn
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Sea bed plumesSea bedHang Hau Forma
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10-Sea bedHang Hau Formation20-OLCD
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West Lamma Channel The Hang Hau For
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corestone boulders. Granite cliffs
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Plate 49 - Feldsparphyric Rhyolite
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Plate 53 - Sheet Joints in Medium-g
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aA /ChekLapKokYUE SHAN(LANTAU ISLAN
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dressing on the foreshore of Sham W
- Page 156 and 157:
Evans, R.B. (1990). Hong Kong Gravi
- Page 158 and 159:
Lee, C.M. (1985). Explanatory notes
- Page 160 and 161:
Whiteside, P.G.D. & Wragge-Morley,
- Page 162 and 163:
Appendix 2Selected Whole-rock XRF G
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Appendix 2 (continued)Sample HK5570
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Appendix 3Microfossils Identified f
- Page 168 and 169:
Appendix 4bSelective normalized pal
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IndexPage numbers in bold refer to
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Hang Hau Formation 25, 115, 118, 12
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San Chau 30, 31, 32, 54San Shek Wan
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This book is due for return or rene