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Field Trip Report - Society of Economic Geologists

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Sweden field trip report: <br />

SEG Student Chapter ETH Zürich <br />

17 th -­‐26 th <strong>of</strong> June 2013 <br />

Stockholm, Sweden was the starting point for the trip around central and northern <br />

Sweden joined by 8 members <strong>of</strong> the SEG Student Chapter Zürich. <br />

Stops on the first day included outcrops and dumps <strong>of</strong> the historic Bästnas and Norberg <br />

mining districts known for REE and Fe-­‐mineralisation in skarns. <br />

On the second day NewBoliden hosted a visit to their Garpenberg “VMS” Zn-­‐Pb-­‐Ag <br />

deposit. Johann Olsson and Michaela Aberg took us on tour along a drift, which showed <br />

different kinds <strong>of</strong> mineralization including later Ag-­‐veinlets crosscutting earlier Zn-­‐ and <br />

Pb-­‐mineralization in skarns. During the afternoon Åsa Erlfeldt and Giovanni Cibrario <br />

were hosting a small discussion round on the larger scale deposits geology. Afterwards <br />

they took us to the core-­‐shed to show us the different metavolcanic and <br />

metasedimentary sequences and different mineralization types in core. <br />

On June 18 th we stopped at outcrops and dumps <strong>of</strong> the Garpenberg area to see the <br />

surface exposure <strong>of</strong> some skarn mineralization and volcanic sequences. In the late <br />

morning we reached the Stollbergsgruva, a historic mine for Ag and Fe. In the afternoon <br />

we made stops to visit the dumps <strong>of</strong> the Grängesberg Fe-­‐oxide-­‐Apatite deposit and old <br />

workings <strong>of</strong> the Kopparberg/Finngruvan Cu workings. <br />

After staying the night at Lake Alvlangen we visited BIF-­‐horizons on the lakeshore and <br />

Accreted Lapilli in the surrounding area. Then we went on our way to the Persberg and <br />

Langban mineral districts, which are famous for their mineral diversity and historic <br />

mining for Fe-­‐skarns. Persberg is furthermore known as the birthplace <strong>of</strong> the term <br />

skarn. <br />

On June 21 st , we went to the Unesco cultural world heritage site at Falun. This historic <br />

mine has been mined for Copper since the 10 th century. The rest <strong>of</strong> the day we used to <br />

reach our destination <strong>of</strong> the day, lake Orsa. <br />

On June 22 nd , we went on a long drive to the north. The destination was the Svartliden <br />

deposit. The employees <strong>of</strong> Dragon mining invited us to their midsummer festivities in <br />

the evening. On the following day Katerina Schloglova introduced us to the Svartliden <br />

Au-­‐mine on the Gold-­‐line. She gave us a detailed overview <strong>of</strong> the different lithologies the <br />

structural control <strong>of</strong> the deposit and gave us a tour around the open pit. After the visit <br />

we set <strong>of</strong> towards Galliväre with a stop at a pegmatite near Jokkmokk with huge feldspar <br />

and biotite crystals. <br />

On June 24 th , Gregory Joslin and S<strong>of</strong>ia Höglund took us around the NewBoliden Aitik Au-­‐<br />

Cu. The day started with an introduction into the deposit characteristics and mining <br />

methods. In the pit they introduced us to the metavolcanic and metasedimentary host <br />

lithologies that were subject to Amphibolite facies metamorphism. Furthermore, they


took us to outcrops <strong>of</strong> later pegmatite veins. The disseminated chalcopyrite and <br />

chalcopyrite-­‐stringer mineralization was also pointed out. Afterwards we were taken <br />

around the processing plant at Aitik with their autogenous mill and flotation plants. <br />

After our visit we drove to our most northern stop <strong>of</strong> the trip at Kiruna. On June 25 th <br />

Kari Niiranen gave us a tour around the largest underground Fe-­‐mine in the world <br />

operated by LKAB. The day started with a presentation about the deposit its different <br />

stratigraphies and mining methods. The underground visit gave an insight into <br />

machinery used in large-­‐scale underground mines and the following tour <strong>of</strong> on <strong>of</strong> the <br />

processing plants explained some <strong>of</strong> the difficulties and advantages <strong>of</strong> mining for <br />

Kiruna-­‐type Magnetite-­‐Apatite ore. The day was rounded <strong>of</strong> with a visit to the core shed <br />

where most significant stratigraphies could be investigated. <br />

On the long drive back to Stockholm from Kiruna we made one final stop at outcrops <strong>of</strong> <br />

the Alnö Carbonatite on the coast <strong>of</strong> the Baltic Sea, one <strong>of</strong> the prime examples for <br />

Carbonatites in Europe. <br />

We would like to thank everyone who has helped us with organizing this field trip. All <br />

mentioned geologists in the visited mines and the associated companies as well as <br />

several geologists familiar with the geology <strong>of</strong> Sweden who gave us precious tips on <br />

which deposits and outcrops to visit and access to older field guides and further <br />

literature (e.g. Erik Jonsson, Hannes Mattsson, Benni Mattsson and Torbjörn Bergmann). <br />

Furthermore, we are grateful for the substantial funding from Data Metallogenica and <br />

the SEG!


Sulfide mineralization in skarn with later veinlets rich in Ag at the Garpenberg mine


Metre-­‐scale biotite and feldspar crystals at a pegmatite near Jokkmokk


The Aitik Au-­‐Cu open-­‐pit mine


Participants <strong>of</strong> the field trip on the arctic circle

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