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Hong Kong Geology Guide Book Geotechnical Engineering Office ...

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Fan Lau, Lantau Island<br />

Introduction<br />

19. Tong Fuk Quartz Monzonite and Fan Lau Granite<br />

The Mesozoic intrusive rocks of <strong>Hong</strong> <strong>Kong</strong> have been classified into four suites that<br />

represent four main phases of intrusive magmatism. These four suites can be<br />

correlated with four major volcanic groups. Although the Tong Fuk Quartz Monzonite<br />

and Fan Lau Granite are different rock types, they both belong to the youngest Lion<br />

Rock Suite. The Tong Fuk Quartz Monzonite occurs intermittently around the<br />

northern and southern margins of the main outcrop of the Upper Jurassic Lantau<br />

Volcanic Group (mainly on the southern margin), and was probably intruded along<br />

ring faults associated with the Lantau caldera. In contrast, the Fan Lau Granite is<br />

exposed only on the Fan Lau peninsula, so can be regarded as a relatively minor body.<br />

Granitic rocks are the second most common rock type in <strong>Hong</strong> <strong>Kong</strong>, with volcanic<br />

rocks covering a larger area. In addition, granite weathers more deeply than the<br />

volcanic rocks. Consequently, outcrops of fresh granite are generally much less<br />

common than those of volcanic rock. However, there are excellent exposures of the<br />

Tong Fuk Quartz Monzonite and the Fan Lau Granite on the Fan Lau peninsula.<br />

Access to Fan Lau, Lantau Island<br />

125

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