张招崇, 周美福, Paul T Robinson, 毛景文, 杨建民, 左国朝. 2001. 北祁连山西段熬油沟蛇绿岩SHRIMP分析结果及其地质意义[J]. 岩石学报, 17(2): 222-226.
[25]
Becker K and Von Herzen R P. 1996. Pre-drilling observations of conductive flow heat flow at the TAG active mound using Alvin[A]. In: Proceeding of ODP[C]. Initial Reports, 158: College Station, TX: 23-29.
[26]
Franklin J M, Sangster D F and Lydon J W. 1981.Volcanic-associated massive sulfide deposits[J]. Econ. Geol., (75th Anniv): 485-627.
[27]
Hall D L, Sterner S M and Bodnar R J. 1988. Freezing point depression of NaCl-KCl-H2O solutions[J]. Econ. Geol., 83(1): 197-202.
[28]
Hutchinson R W. 1984. Massive sulphide deposits and their significiance to other ores[A]. Paper for fifth regional congress on geology, mineral and energy resources of southeast Asia[C]. Information Institute of Geological Ministry. 22-27.
[29]
Ohmton H. 1983. Stable isotope geochemistry of ore deposits[J]. Review of Minerology, 16: 491-560.
[30]
Sangster D F and Scott S D. 1976. Precambrian Statabound, massive Cu-Zn-Pb sulfide deposits of North America[A]. Wolf K A, ed. Handbook of strata-bound and stratiform ore deposits[C]. Amsterdam: Elsevier. 129-222.
[31]
Spooner E T C and Bray C J. 1977. Hydrothermal fluids of seawater salinity in ophiolite sulphide ore deposits Cyprus[J]. Nature, 266: 808-812.
