正构烷烃的成矿意义——以广西田林高龙卡林型金矿为例

胡明安

Volume 28 Issue 3

May 2003

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HU Ming-an, 2003. Tracer Significance of Normal Alkane for Gold Mineralization of Gaolong Carlin Type Gold Deposit. Earth Science, 28(3): 301-305.

Citation:

HU Ming-an, 2003. Tracer Significance of Normal Alkane for Gold Mineralization of Gaolong Carlin Type Gold Deposit. Earth Science, 28(3): 301-305.

HU Ming-an, 2003. Tracer Significance of Normal Alkane for Gold Mineralization of Gaolong Carlin Type Gold Deposit. Earth Science, 28(3): 301-305.

Citation:

HU Ming-an, 2003. Tracer Significance of Normal Alkane for Gold Mineralization of Gaolong Carlin Type Gold Deposit. Earth Science, 28(3): 301-305.

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Tracer Significance of Normal Alkane for Gold Mineralization of Gaolong Carlin Type Gold Deposit

HU Ming-an

Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2002-05-29
Publish Date: 2003-05-25

Abstract

Abstract

Gaolong Carlin type gold deposit is situated in the nucleus of the Gaolong arch in the western section of the Xilin-Baise fault-fold zone. The ore bodies are placed in the contact of the Carboniferous-Permian carbonites and the Triassic turbidites. The Baise-Gaolong Guzhang regional large-scale faults and their secondary structures form the passages for the flow of the mineralizing fluid and the spaces for the precipitation of the mineralized materials. There are four types of normal alkanes in the Gaolong ore district: the normal maturation type in the non-mineralized strata, and the abnormal maturation type, the hydrothermal solution type and the microbial degradation type in the ore bodies. These normal alkanes offer the favourable mineralization information and have the tracer significance for the gold mineralization.
- normal alkane,
- Carlin type gold deposit,
- mineralization information,
- tracer significance,
- Gaolong of Guangx

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References(9)

References

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