Use of cookies

Lund University uses cookies to ensure that the website functions properly and to improve your experience.

Read more in our cookie policy

Search results

Filter

Reset filter

Filetype

Your search for "*" yielded 548952 hits

Laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS)

The laboratory is equipped with a Bruker Aurora Elite ICP-MS and a 193 nm Cetac Analyte G2 excimer laser installed with a two volume HelEx2 sample cell. LA-ICP-MS  is a powerful method for element analysis in a wide variety of solid materials (i.e. minerals, bone & teeth materials, wood, ceramics, etc.) at spatial resolutions from a few up to several hundred µm. Quantitative analyses can be obtain

https://www.geology.lu.se/research/laboratories-equipment/laser-ablation-inductively-coupled-plasma-mass-spectrometry-la-icp-ms - 2025-11-09

Programme structure

Master courses Our MSc. programme has one entry with a suggested study path according to the scheme below. When you are admitted, you are automatically admitted to the first two courses. The first course, Methods in geosciences (GeoM20), is compulsory. However, within the limitations of the degree requirements (see below) – and the periods of the year when the courses are given – you can tailor yo

https://www.geology.lu.se/education/programme-structure - 2025-11-09

Application for non-exchange students

Apply at www.universityadmissions.seAll information about the application procedure and requirements can be found on this site.Note that after having arrived in Lund and started on your first course you need to apply for admission to courses during your following study terms (even if you have already been given admission to our Master programme). This is done every term through www.universityadmis

https://www.geology.lu.se/education/application-non-exchange-students - 2025-11-09

Prices

The cost per sample varies considerably depending on sample size, lithology and necessary further treatment of the residues. Please contact us for an estimate.The sample residues will be delivered in dry state and sub-divided into different fractions, normally one light and one heavy fraction (the latter of which contains phosphatic fossils). As a rule our finest sieve is 63 um. If you would like

https://www.geology.lu.se/research/laboratories-equipment/lund-university-microfossil-laboratory/prices - 2025-11-09

Application for exchange students

The term exchange student implies that your home university has a formal agreement to exchange students with Lund University. The agreement can be general/central and open to all the university's students or limited to a specific department or faculty. In either case you must first apply for the exchange at your home university; either through your central International Office or through an intern

https://www.geology.lu.se/education/application-exchange-students - 2025-11-09

The Student Council for Physical Geographers and Geologists (SNG)

SNG is an organization run entirely by students at INES (Physical Geography department) and the Geology Department. It represents students in the decision-making boards of the two departments and at the Faculty of Science (LUNA). This provides students an opportunity to give feedback about their education, comment on new ideas and suggest ways to make the quality of education even better. It also

https://www.geology.lu.se/education/student-organisations/student-council-physical-geographers-and-geologists-sng - 2025-11-09

Events

Current and upcoming events PhD-course in Hydrogeological Conceptual Models for Groundwater Use and Protection. Characterisation methods and scaling considerations, 4.5 credits 15th-31st of March 2023 Two days of field method demonstration and an afternoon of lectures about FLUTe-liner technology methods, 17th - 28th of March Passed events 12th International Eclogite Conference Mosasaur Meeting V

https://www.geology.lu.se/research/events - 2025-11-09

Mosasaur Meeting V

  Abstract volume The abstact volume is avalable for download here   Third Circular 5th Triennial Mosasaur Meeting – a global perspective on Mesozoic marine amniotes   Museum of Evolution, Uppsala University Uppsala, Sweden May 16–20, 2016   Dear Friends and Colleagues, The 5th Triennial Mosasaur Meeting (http://www.geology.lu.se/mmv) is now less than two months away and it is time to update you w

https://www.geology.lu.se/research/events/mosasaur-meeting-v - 2025-11-09

borttagen - 40Ar/39Ar Geochronology Laboratory

The 40Ar/39Ar method is a tremendously versatile and powerful geochronometer which has been used to date K-bearing rocks and minerals as young as a few 10’s of thousands of years to the oldest rocks on Earth. Argon for 40Ar/39Ar analysis can be released either by step-heating a sample (single grain or rock aggregate) using a furnace or a defocused laser and by in-situ Laser Ablation of a small ≥ 2

https://www.geology.lu.se/borttagen-40ar39ar-geochronology-laboratory - 2025-11-09

Equipment

The main components of the 40Ar/39Ar lab at the University of Lund consist of a Micromass-5400 Gas Source Mass Spectrometer with a faraday and an electron multiplier. A custom designed and built UHV gas metal extraction line, which contains two SAES C50-ST101 Zr-Al getters and a cold finger cooled to ca –155°C by a Polycold P100 cryogenic refrigeration unit. For gas extraction, the 40Ar/39Ar labor

https://www.geology.lu.se/research/laboratories-equipment/equipment - 2025-11-09

Publications

Sandström, B., Tullborg, E.-L. Larson, S.-Å., & Page, L.M., (In Press) Brittle tectonothermal evolution in the Forsmark area, central Fennoscandian Shield, recorded by paragenesis, orientation and 40Ar/39Ar geochronology of fracture minerals. TectonophysicsDrake, H., Tullborg, E.-L., & Page, L.M., (In Press) Distinguished multiple events of fracture mineralization related to far-field orogenic eff

https://www.geology.lu.se/research/laboratories-equipment/publications - 2025-11-09

News

News5 January 2011: We are happy to announce that the lab has established a new collaboration with the www.supercontinent.org project. The Lund lab will date young or badelleyite free mafic rocks.9 September 2010: Ms. Jill Gabo will be working in the lab 2 1/2 months a guest researcher to to date volcanism in the Philippines.7 October 2009: We are happy to announce that Dr. Laurence Page will star

https://www.geology.lu.se/research/news - 2025-11-09

Mineral Separation Laboratory

Efficient techniques for mineral separation are important in almost all geochronological studies. From year 2000, we have used the so called “water-based technique (pdf, new tab)” for separation of baddeleyite (and zircon). Baddeleyite is a reliable geochronometer for dating the crystallization of mafic and other silica-undersaturated rocks. The technique is based on the observation that small gra

https://www.geology.lu.se/research/laboratories-equipment/mineral-separation-laboratory - 2025-11-09

Equipment

1. Circa 0,5 kg sample is sawed in 1-cm thick slices using an ordinary slab saw.    2. After washing and drying, the slices are reduced in size to cm-large pieces by using a small sledge hammer.   3. In order to get a very fine-grained sample (almost powder), we use a small swing mill.   4. After adding some water, the sample is loaded in ca. 50 g portions on a Wilfley-Holman 700 water-shaking tab

https://www.geology.lu.se/research/laboratories-equipment/mineral-separation-laboratory/equipment - 2025-11-09

Publications

Söderlund, U. and Johansson, L., 2002. A simple way to extract baddeleyite (ZrO2), Geochem. Geophys. Geosyst., 3(2), 10. 1029/2001GC000212 (Technical brief), 2002. (pdf, new tab)Söderlund, U., Isachsen, C., Bylund, G., Heaman, L., Patchett. P.J., Vervoort, J.D. and Andersson, U.B., 2005. U-Pb baddeleyite ages and Hf, Nd isotope chemistry constraining repeated mafic magmatism in the Fennoscandian S

https://www.geology.lu.se/research/laboratories-equipment/mineral-separation-laboratory/publications - 2025-11-09