DEPOSITIONAL FACES OF THE ZHUJIANG DELTA FROM FOSSIL DIATOM

HUANG ZHENGUO; ZONG YONGQIANG; HE RUIRU; QI YUZAO; LIN LANYING; ZHANG ZIAN

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Article Navigation > Acta Oceanologica Sinica > 1987 > (2): 222-228

HUANG ZHENGUO, ZONG YONGQIANG, HE RUIRU, QI YUZAO, LIN LANYING, ZHANG ZIAN. DEPOSITIONAL FACES OF THE ZHUJIANG DELTA FROM FOSSIL DIATOM[J]. Acta Oceanologica Sinica, 1987, (2): 222-228.

Citation:

HUANG ZHENGUO, ZONG YONGQIANG, HE RUIRU, QI YUZAO, LIN LANYING, ZHANG ZIAN. DEPOSITIONAL FACES OF THE ZHUJIANG DELTA FROM FOSSIL DIATOM[J]. Acta Oceanologica Sinica, 1987, (2): 222-228.

HUANG ZHENGUO, ZONG YONGQIANG, HE RUIRU, QI YUZAO, LIN LANYING, ZHANG ZIAN. DEPOSITIONAL FACES OF THE ZHUJIANG DELTA FROM FOSSIL DIATOM[J]. Acta Oceanologica Sinica, 1987, (2): 222-228.

Citation:

HUANG ZHENGUO, ZONG YONGQIANG, HE RUIRU, QI YUZAO, LIN LANYING, ZHANG ZIAN. DEPOSITIONAL FACES OF THE ZHUJIANG DELTA FROM FOSSIL DIATOM[J]. Acta Oceanologica Sinica, 1987, (2): 222-228.

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DEPOSITIONAL FACES OF THE ZHUJIANG DELTA FROM FOSSIL DIATOM

1.
Guangzhou Institute of Geography, Guangzhou
2.
Department of Biology, Jinan University, Guangzhou

Received Date: 1985-10-30
Rev Recd Date: 1986-04-09

Abstract

Abstract

Fossil diatom groups from 85 samples of drill holes and 13 samples of the known depositional environment are analysed. The boundary of the Zhujiang Delta is discussed from the distribution of fossil diatom. The horizonal variation of Holocene sedimentary facies can be divided into four kinds of depositional environment corresponding to the delta plain subfacies and the delta front subfacies. The vertical variation of Holocene depositional facies shows twice changes of transgression from weak to vigorous.

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