Characteristics and provenance of main detrital minerals in the Prydz Bay,Antarctic

Liu Yiying; Jin Bingfu; Chen Zhihua; Wang Kunshan

doi:10.3969/j.issn.0253-4193.2016.05.009

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Liu Yiying, Jin Bingfu, Chen Zhihua, Wang Kunshan. Characteristics and provenance of main detrital minerals in the Prydz Bay,Antarctic[J]. Haiyang Xuebao, 2016, 38(5): 96-107. doi: 10.3969/j.issn.0253-4193.2016.05.009

Citation:

Liu Yiying, Jin Bingfu, Chen Zhihua, Wang Kunshan. Characteristics and provenance of main detrital minerals in the Prydz Bay,Antarctic[J]. Haiyang Xuebao, 2016, 38(5): 96-107. doi: 10.3969/j.issn.0253-4193.2016.05.009

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Characteristics and provenance of main detrital minerals in the Prydz Bay,Antarctic

doi: 10.3969/j.issn.0253-4193.2016.05.009

1.
Institute of Coast, Ludong University, Yantai 264025, China
2.
The First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China

Received Date: 2015-06-10

Abstract

Abstract

The depositional environment and sedimentary provenance were studied in the Prydz Bay based on mineralogical analysis of 33 surface sediment samples. Seventeen types of heavy minerals were recognized in this study. Garnet,hornblende and magnetite are the dominant heavy minerals,hypersthene and hematite are the characteristic minerals. From the distribution of the mineral assemblages,four mineral provinces can be identified. In Fram Bank mineral province (Province I),the garnet is treated as the main mineral and has the highest content of heavy mineral. In Prydz channel mineral province (Province II),the magnetite is treated as the diagnostic mineral,garnet and epidote take a dominant position of the minerals. In Four Ladies Bank province (Province Ⅲ) has significant content of hypersthene. In deep slope mineral province (Province Ⅳ),the main mineral is hornblende and the garnet is less than other provinces. The mineralogical characteristics of garnets from the study area shows that, the clastic garnet contains higher Fe,Mg element and lower Ca,Mn element,and mainly comes from senior granulite facies. Detrital mineral distribution characteristics is controlled by provenance,the current system and glacier activities such as a product of the combined action of multiple factors.
- detrital minerals,
- garnet,
- sediments,
- Prydz Bay

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References(49)

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