fresh is pleochroic, varying from light brown to green. Accessory minerals include zircon, titaniteand allanite which is commonly altered.Age RelationsDie fine- to medium-grained granite is considered to be a textural variant of medium-grainedgranite exposed on Lantau Island and is, therefore, presumed to be of similar age. On Chek LapKok, the fine- to medium-grained granite probably cooled before the fine-grained granite exposedin the west of the island.m B 9:^ ^ r\ i -Plate 24 - Fine to Medium-grained Granite (11309 17165), from a Borehole South of Ha Law WanFine-grained GraniteDistribution andLithologyFine-grained granite within the district can be divided into megacrystic and non-megacrysticvarieties. The richly megacrystic varieties generally occur adjacent to, or within, gradationalcontact zones with porphyritic, fine- to medium-grained granite and porphyritic, medium-grainedgranite, whereas the non-megacrystic varieties generally occur as separate intrusive bodies.Megacrystic varieties may also occur as textural variants within feldsparphyric rhyolite dykes.Fine-grained granite in the district occurs mainly on Tsing Yi, in and around Ma Wan and thenorthern part of Lantau Island, in central Lantau Island, on Chek Lap Kok and at Sha Lo Wan.Smaller exposures are found on many of the offshore islands.
The granite on Chek Lap Kok is mostly fine grained, and locally includes a noticeablyfiner-grained microgranite. All the varieties are characterized by an inequigranular groundmass,with a wide range of grainsizes seen in hand specimen and thin section.DetailsTsing Yi. On Tsing Yi, fine-grained granite occurs either as a chilled margin to the medium-grained granite, or asrelatively small, discrete, sheet-like intrusions. In each case the rock is pale pink or pinkish-grey, sparselymegacrystic and hypidiomorphic. In some areas, such as south of Cheung Hong Estate (2860 2313), richlymegacrystic, fine-grained granite occurs as textural variants within dykes of feldsparphyric rhyolite which arethemselves either richly or sparsely feldsparphyric. Such occurrences were also noted on Ma Wan for examplesouth of Tung Wan (2461 2327, 2453 2368).On the peak west of Chun Fa Lok (2863 2190), medium-grained granite is cut by a subhorizontal sheets offine-grained granite. The fine-grained granite sheets are chilled against the overlying medium-grained granite butgrade down, through richly megacrystic fine-grained granite, into typical equigranular medium-grained granite(2871 2177). A number of feldsparphyric dykes intrude the granite to the northeast of Chun Fa Lok (2853 2195)and around Nam Wan (2846 2157) and Nam Wan Kok (2886 2123).Fine-grained granite forms a relatively thin (c. 25 m) roof contact zone to the medium-grained granite on the mainridge of Tsing Yi, from northwest of Tai Shan Ha (2827 2300) to above Chun Fa Lok (2854 2207) and westwardsfrom there. The contacts are well exposed on the peak (2847 2273), and to the south (2850 2243) where gradationsfrom equigranular medium-grained granite to megacrystic fine-grained can be seen.Southwest of Nam Wan (2749 2119, 2756 2112, and 2784 2134), megacrystic fine-grained granite forms gentlydipping sheets, or dykes, which appear to coalesce when traced eastwards.South of Cheung Hong Estate, in the centre of Tsing Yi, fine-grained granite, with a markedly megacrystic andinequigranular texture, forms a poorly defined mass that may partly represent the chilled roof margin of a pluton,and partly a dyke-like extension upwards into the overlying country rock. East of these outcrops, sparselymegacrystic fine-grained granite forms a dyke 50 m wide. It cuts the medium-granite along a roughly easterly trend,and is traceable for over 500 m.In northwestern Tsing Yi, sparsely megacrystic fine-grained granite has been noted in numerous localities. Mostoutcrops appear to be dykes intruding feldsparphyric rhyolite dykes. In cut-slopes (2801 2272) east of Sai Tso Wan,fine-grained granite dykes are intruded into crystal tuff.In the southwest of the island, west of the Power Station (2760 2130), and in the north around Cheung HongEstate, the medium-grained granite has been modified texturally to form richly megacrystic., fine-grained granitealong the contact with sparsely megacrystic, fine-grained granite. Modified textures were also noted in the OilDepot (2924 2244) at Tai Shan Ha,Ma Wan. On Ma Wan, fine-grained granite is exposed along the shore between Tai Pai Tsui (2415 2264) andNam Wan (2446 2273), and on the shore east of Pak Nai Shan (2470 2289). The contact between the fine-grainedgranite and the country rock to the west of Tai Pai Tsui is faulted, whereas to the east it is intruded by a basaltdyke. This margin may also be faulted. A gently dipping intrusive contact is exposed east of Pak Nai Shan but alittle further north, fine- to medium-grained granite is in direct contact with the tuff; the contact is sharp andgeometrical as if a large polygonal block had foundered in the granite magma. Fifty metres north of this contact, afine-grained granite dyke intrudes the fine- to medium-grained granite and can be traced offshore onto rocky islets,where it separates the fine- to medium-grained granite from the tuff.In the north of Ma Wan near Cheung Tsui (2453 2366), Tarn Shui Wan (2395 2357) and Shek Tsai Wan (23672336) fine-grained granite forms a core facies to sparsely feldsparphyric rhyolite dykes.The fine-grained granite forms a major part of Tang Lung Chau but the shape of the intrusion is obscure as mostcontacts with country rocks are faulted, or interrupted by later intrusions.Sha Chau. Strongly megacrystic, fine-grained granite is exposed north and west of the temple (064 232) on ShaChau. The granite has tabular feldspar megacrysts, up to 50 mm long, which are set in a fine- to very fine-grainedgroundmass. Texturaily, this granite is similar to that exposed on the east side of Castle Peak (Tsing Shan; Sheet5).Penny's Bay. An exposure (2178 1938) on the southwest side of the bay comprises fine-grained granite which iscut by thin, iiregular basalt dykes, Both the granite and the basalt are cut by a feldsparphyric rhyolite dyke. About71
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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
- 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
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- Page 85 and 86: the Lantau Formation, however, and
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- Page 91 and 92: Silver Mine Bay. On the headland so
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- Page 98 and 99: Pre-Yensfaanlan StructureWithin the
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- Page 102 and 103: NeotectonicsFault activity in the r
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- Page 107 and 108: the majority of rocks in the distri
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- Page 114 and 115: trains. The regolith on most steep
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Plate 48 - Sandy Beach at Fan Lau S
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Pre-Chek Lap Kok Formation Deposits
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formation. The sequence is usually
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BOREHOLE NO: ESC 17GRID REFERENCE:
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BOREHOLE NO: A5/1GRID REFERENCE: 80
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formation, thinly laminated clays o
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Quinqueloculina seminulum, which is
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Channel and Transgressive Deposits.
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Figure 20 - Areas of Acoustic Turbi
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West Lamma Channel These may be att
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Figure 23 - Depth-Averaged, Maximum
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The formation is Holocene in age. T
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Boreholes (A5/1, A5/2, B2/1, ESC17
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Plate 51 - Deep Weathering Profile
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Chapter 10Economic GeologyIntroduct
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Non-metalliferous MineralsFissure v
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REFERENCESAddison, R. (1986). Geolo
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James, J.W.C. (1993). The offshore
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Sewell, R.J., Strange, PJ., Langfor
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Appendix 1Microfossils identified f
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Appendix 2 (continued)Sample HK9913
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Appendix 2 (continued)Sample HK1054
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Appendix 4aSelective normalized pal
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,Appendix 5 -Radiocarbon and Other
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construction materials 151contact m
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molybdenite 149Mong Tung Hang 151Mo
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talus 107,115Tarn Tsui Wan 71,87Tan
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LB 555.125 G34 LGeology of Lantaii