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Berry, Leonard, Ruxton, Bryan P. (1957) Structure and Form of Cheung Chau Island, Hong Kong. Geological Magazine, 94 (3) 249-260 doi:10.1017/s0016756800068618

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Reference TypeJournal (article/letter/editorial)
TitleStructure and Form of Cheung Chau Island, Hong Kong
JournalGeological Magazine
AuthorsBerry, LeonardAuthor
Ruxton, Bryan P.Author
Year1957 (June)Volume94
Issue3
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0016756800068618
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Mindat Ref. ID248668Long-form Identifiermindat:1:5:248668:4
GUID0
Full ReferenceBerry, Leonard, Ruxton, Bryan P. (1957) Structure and Form of Cheung Chau Island, Hong Kong. Geological Magazine, 94 (3) 249-260 doi:10.1017/s0016756800068618
Plain TextBerry, Leonard, Ruxton, Bryan P. (1957) Structure and Form of Cheung Chau Island, Hong Kong. Geological Magazine, 94 (3) 249-260 doi:10.1017/s0016756800068618
In(1957, June) Geological Magazine Vol. 94 (3) Cambridge University Press (CUP)
Abstract/NotesAbstractA study of Cheung Chau Island has revealed a close adjustment between the form of the island and the geological structure. The island is made up of dominant granite cut by granite-porphyry and dolerite dykes, which are affected by later faulting. A theory of progressive emergence is put forward for the denudation chronology of the area and the various forms related to the former submergence have been mapped. The relation of coastal and inland forms to structure is considered, and the evolution of the coast is outlined.


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