Paleomagnetism Geomagnetism

 
 

Paleomagnetic Laboratory – IDL

The Paleomagnetic Laboratory – IDL has more than 30 years of supporting research in the areas of paleomagnetism, secular variation, magneto-stratigraphy, archeomagnetism, rock magnetism and anisotropy of magnetic susceptibility and geomagnetism. The research and studies have been related to the rock formation and deformational processes linked to tectonics, as well as paleogeography, paleoenvironment, and environmental magnetism. This laboratory has also provided training and made it possible for many students to obtain academic degrees.

The laboratory is integrated in the C4G (Collaboratory for Geosciences) and EPOS (European Plate Observing System) thematic core services Multi-scale laboratories

 
 

Equipment

The laboratory is equipped with instruments for paleomagnetism, mineral and fabric-magnetic analysis, and geomagnetic surveys, as:

Paleomagnetism – Spinner magnetometer (AGICO), AF demagnetizer (AGICO), thermal demagnetizer (home build);

Rock magnetic characterization – Kappabridge with a furnace and cryostat (AGICO), anhysteretic magnetizer (AGICO), pulse magnetizer (ASC);

Geomagnetism (field, surface and aerial survey) – G 858 MagMapper magnetometer (Geometrics), MagDrone R3 magnetometer (Sensys) + UAV hexacopter (DJI);

Fluxgate magnetometer MAG 01-H (Bartington);

Also complete equipment for fieldwork, sample preparation and auxiliary equipment for field and laboratory work.

 

Paleomagnetism and Rock Magnetic Characterization

Spinner Magnetometer

Spinner Magnetometer JR6 (AGICO); This is a dual speed (16.7 Hz or 89.7 Hz) spinner magnetometer  using induction coils. It  measures the remanent magnetization (vectorial) of rock specimens, with a sensitivity range of 10e-6 A/m to 10e+4 A/m.

JR-6 Spinner Magnetometer (agico.com)

Alternating Field Demagnetizer and Anhysteretic Magnetizer

LDA 3: this instrument demagnetizes rock or sediment specimens with an alternating field up to 200 mT. It is possible to demagnetize cores or cubes up to 2.5 cm in diameter.

AMU 1: this device imparts an anhysteretic remanant magnetization (ARM) in a d.c. field up to 500 μT or an isothermal remanent magnetization in a d.c. field up to 200 mT. It can be used to magnetize cores or cubes up to 2.5 cm in diameter. Useful for magnetic grain size characterization. This device is used in conjunction with the AGICO LDA 3 AF demagnetizer and JR6 magnetometer.

LDA3-A manual (PDF)

 

Thermal Demagnetizer

Custom-made shielded magnetic furnace (maximum T~700ºC).

This furnace allows thermal demagnetization of up to 8 paleomagnetic samples under conditions of negligible magnetic field. Demagnetization takes place in 2 chambers, one for heating and one for cooling the samples.

Impulse Magnetizer

IRM Impulse Magnetizer IM-10-30 (ASC Scientific).

This instrument is designed to produce short duration high field pulses to magnetize standard paleomagnetic samples (IRM acquisition). It has 4 coils: Coil #1 can produce fields ranging from 30 to 600 Gauss (3 to 60 mT), coil #2 fields range from 0.5 to 11 kGauss (50 mT to 1.1 T), coil #3 ranges from 1.5 a 27 kG (150 mT to 2.70 T) and coil #4 can apply fields from 3 to 50 kG (300 mT to 5 T).

ASC Impulse Magnetizers – ASC Scientific

 
 
 

Susceptibility Meter

Three frequency multifunction KAPPABRIDGE, MFK1-FA + High Temperature Furnace and Low Temperature Cryostat,  (AGICO).

The instrument measures bulk susceptibility, anisotropy of magnetic susceptibility (AMS), and susceptibility between -196ºC and 20ºC (CS-L adapter) and between 20ºC and 700ºC (CS-3 adapter). Bulk susceptibility and AMS can be measured on cores and cubes up to 2.5 cm in diameter. AMS can be measured using an automatic rotator. AMS is useful for qualitatively describing magnetic fabrics in rocks, sediments and glacial deposits. Susceptibility versus temperature measurements can be used to identify the magnetic mineralogy of a specimen and its propensity to alter. High and low temperature measurements can be run in air or argon. Sample chips or powders of a variety of materials can be measured.

MFK1 Kappabridge (agico.com)

 

Geomagnetic Survey Equipment

 
 

Magnetometer G-858 Geometrics 

This is a high sensitivity, fast-sampling ‘walking’ magnetometer.

The principle of operation of this magnetometer is a self-oscillating split-beam Cesium Vapor (non-radioactive Cs-133); Noise < 0.008 nT/Hz, max sample rate: 10 Hz. Sensitivity: 0.05 nT (at 0.1 Hz) to 0.01 nT (at 1.0 Hz).

G-858 MagMapper Magnetometer – Geometrics : Geometrics

 
 

Magnetometer MagDrone R3 Sensys

Portable magnetometer survey system to be attached to any UAV/drone.

The system consists of an ultra light weight sensor tube with two built-in 3-axis Fluxgates (FGM3D/75) sensors, a data logger (data acquisition at 200 Hz) with internal SD card, rechargeable batteries and an integrated GPS. Resolution is aprox. 150pT.

MagDrone R3 – SENSYS Magnetometer

 
 

Fluxgate Magnetometer MAG 01-H Bartington

The Mag-01H is a portable high performance instrument that provides precision measurements of the direction and intensity (single axis) of magnetic fields from 0.1nT (1µG) to 2,000µT (20G) with a frequency response of DC to 10Hz.

Mag-01H Single Axis – Bartington Instruments

 
 

Students that worked here

 

Henrique Freitas (Universidade de Lisboa, Faculdade de Ciências, Departamento de Engenharia Geográfica, Geofísica e Energia). March to June 2023. (coordinated by Mário Moreira). Subject: Análogos de Marte: à descoberta de basaltos da Terra com propriedades magnéticas análogas a rochas de Marte.

Lisa Grifonni (Università degli Studi di Siena – UNISI), February to June 2023 (coordinated by Mário Moreira). Subject: Measuring low field, frequency dependent, magnetic susceptibility and IRM/SIRM of lichens to evaluate environmental contamination of metallic particulate matter (PM) in exploratory project in Lisbon.

Inês Rodrigues (Universidade de Lisboa, Faculdade de Ciências, Departamento de Engenharia Geográfica, Geofísica e Energia). March to June 2022. (coordinated by Mário Moreira). Subject: Assinatura magnética em cascas de plátano – contribuição para a biomonitorização da contaminação ambiental por partículas metálicas finas.

Jeremy Thouvenin (Université de Strasbourg). June-July 2022. (coordinated by Mário Moreira). Subject: Determination of AMS (anisotropy of magnetic susceptibility) and characterization of the magnetic fabric of a collection of 10 dikes from the Fogo volcano to deduced magmatic flow orientations.

 

Useful links

  • Paleomagnetic Data  (NGDC / WDC Boulder, NOAA)

  • Magnetic Field Calculator (NGDC/NOAA)

  • MagIC – Magnetics Information Consortium – The Magnetics Information Consortium (MagIC) improves research capacity in the Earth and Ocean sciences by maintaining an open community digital data repository for rock and paleomagnetic data with portals that allow users to archive, search, visualize, download, and combine these versioned datasets. MagIC supports the international rock and paleomagnetic communities and endeavors to bring data out of private archives, making them accessible to all and (re-)useable for new, creative, collaborative scientific and educational activities.

  • GEOMAGIA database  – GEOMAGIA is an international collaboration to provide easy access to published archeomagnetic/volcanic and sediment paleomagnetic and chronological data for the past 50 ka. It has been funded by the National Science Foundation (NSF and the German Research Foundation (DFG) SPP 1488 and is or has been supported by the following institutions: GFZ Potsdam, University of California San Diego, University of Freiburg, University of Liverpool and the University of Helsinki.

  • IRM – Institute for Rock Magnetism

e-Book links

Contact and Management 

Facility manager: Mário Moreira | mamoreira@fc.ul.pt;   mario.moreira@isel.pt
Pedro Silva | pmfsilva@fc.ul.pt;   pedro.fsilva@isel.pt

Address

Instituto Dom Luiz – Paleomagnetic Laboratory
Faculdade de Ciências da Universidade de Lisboa
Campo Grande Edifício C1, Piso 1, (sala/room 1.1.26)
1749-016 Lisboa, Portugal