Hydrothermal circulation at 1.8 Ga in the Kiruna area, northern Sweden, as revealed by apatite geochemical systematics

Author:

Yan Shengchao,Wan BoORCID,Andersson Ulf B.

Funder

National Natural Science Foundation of China

National Key Research and Development Program of China

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference75 articles.

1. Andersson, U.B., Rutanen, H. 2016. Geological features in and around the Kiirunavaara ore body, northernmost Sweden, and some implications. In International Geological Congress. Cape Town. Paper 2989.

2. Structural Evolution of the Central Kiruna Area, Northern Norrbotten, Sweden: Implications on the Geologic Setting Generating Iron Oxide-Apatite and Epigenetic Iron and Copper Sulfides;Andersson;Econ. Geol.,2021

3. 1.8 Ga magmatism in the Fennoscandian Shield; lateral variations in subcontinental mantle enrichment;Andersson;Lithos,2006

4. Andersson, U.B., Zack, T., Aupers, K., Blomgren, H., Hogmalm, J., et al. 2016. Ages of hydrothermal overprints in the Kiruna iron oxideapatite ores as recorded in secondary monazite and xenotime. 35th International Geological Congress, At: Cape Town, Paper Nr. 3431.

5. Andersson, U.B., Menard, D.S., Majka, J. 2022b. Uranium mineralizations in Kiirunavaara, Sweden. In 150 Years Anniversary Meeting of the Geological Society of Sweden. , pp. 348-49. Uppsala, Sweden, Special Publication 1.

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