Results 31 to 40 of about 749 (183)

Cool deltas: Sedimentological, geomorphological and geophysical characterization of ice‐contact deltas and implications for their reservoir properties (Salpausselkä, Finland)

open access: yesSedimentology, Volume 68, Issue 7, Page 3057-3101, December 2021., 2021
Abstract Sediments deposited by glacial meltwaters (for example, ice‐contact delta deposits) form permeable packages in the subsurface that can act as reservoirs for both water and hydrocarbons. They are also an important source of aggregate for the construction industry.
Bartosz KurjaŃski   +10 more
wiley   +1 more source

Detrital zircon geochronology of Paleoproterozoic metasedimentary rocks from Jämsä, Central Finland [PDF]

open access: yesBulletin of the Geological Society of Finland
In this short communication, we present new detrital single grain zircon U-Pb data for six metasedimentary rock samples from Jämsä, Central Finland.
Perttu Mikkola   +2 more
doaj   +1 more source

On the microfossils of Corycium enigmaticum [PDF]

open access: yesBulletin of the Geological Society of Finland, 1969
This paper deals with alga-like microfossils found in the about 2 000 m.y. old schist belt situated N of Tampere, SW Finland and belonging to the lower Svecofennian.
A. Matisto
doaj   +1 more source

Zircon dating of the basalt and felsic dyke in Haveri, SW Finland [PDF]

open access: yesBulletin of the Geological Society of Finland, 2022
The E-MORB type Haveri basalt differs from the volcanic arc type rocks in the Tampere belt showing no subduction signature. It is considered to have formed in a marginal basin prior to the volcanic arc. We present here zircon U-Pb dating on two samples.
Jaakko Kara   +2 more
doaj   +1 more source

Reconstructing craton‐scale tectonic events via in situ Rb‐Sr geochronology of poly‐phased vein mineralization

open access: yesTerra Nova, Volume 33, Issue 5, Page 502-510, October 2021., 2021
Abstract Fault‐ and fracture‐hosted multi‐stage mineral assemblages that formed by fracture reactivation and fluid migration, constitute archives of the tectonic evolution of Precambrian cratons. Complex intergrowth patterns of these mineral records often hinder absolute dating of mineralization events for geological models.
Mikael Tillberg   +5 more
wiley   +1 more source

The Salittu Formation in southwestern Finland, part I: Structure, age and stratigraphy [PDF]

open access: yesBulletin of the Geological Society of Finland, 2016
Because of the relatively low metamorphic grade, low strain and well-preserved early structures in volcanic and volcaniclastic rocks, the Orijärvi triangle (in the center of the larger Orijärvi area) is one of the few locations in the Svecofennian orogen
M. Nironen, I. Mänttäri, M. Väisänen
doaj   +1 more source

Northern landscapes in transition: Evidence, approach and ways forward using the Krycklan Catchment Study

open access: yesHydrological Processes, Volume 35, Issue 4, April 2021., 2021
The Krycklan Catchment Study (KCS, www.slu.se/Krycklan) is located in the heart of the Boreal region in northern Sweden. The field research infrastructure that started in 1980 consists of a 6790 ha catchment, and currently includes 10 long‐term monitored streams, ca.
Hjalmar Laudon   +10 more
wiley   +1 more source

The Luusika potential field anomaly, eastern Estonia: modelling results [PDF]

open access: yesEstonian Journal of Earth Sciences, 2018
This study considers the anomalous gravity and magnetic fields in the Alutaguse petrological–structural domain, eastern Estonia. A 10 km wide local maximum (+6.26 mGal) Bouguer anomaly field was discovered at 58.96°N, 26.61°E from the ground gravity data
Marija Dmitrijeva   +2 more
doaj   +1 more source

Tracing the SW border of the Svecofennian Domain in the Baltic Sea region: evidence from petrology and geochronology from a granodioritic migmatite [PDF]

open access: yes, 2022
Geological investigations of a part of the crystalline basement in the Baltic Sea have been performed on a drill core collected from the depth of 1092-1093 m beneath the Phanerozoic sedimentary cover offshore the Latvian/Lithuanian border. The sample was
Woodard Jeremy   +2 more
core   +1 more source

Development of an in-situ magmatic dome (Svecofennian accretionnary orogen, Finland)

open access: yes, 2014
This study focuses on the formation of the 100 km wide Vaasa magmatic dome (Svecofennian orogen, Finland). It is cored by diatexite migmatites and granitoids and gradually mantled by metatexite migmatites and mica schist.
Hölttä, Pentti   +2 more
core   +2 more sources

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