Lots of new stuff going on...
The end of May saw my last contributions to the FIRE-ATT project at the Insitute of Seismology. During the past nine months I contributed to five external pieces and four conference papers on the OpenFIRE project and presented the application and the project in five conferences and other marketing forums.
Bulk of the project on my behalf is, however, still unpublished as the full version of the application is not yet released and the geological descriptions that were my main responsibility in the OpenFIRE are going to be out only when it happens. You can still check out the beta (or the full version when it gets released) here.
Anyways, good times, but now it's time to move on to other things.
Starting from the beginning of June I have returned to the Division of Geology and Geochemistry. First as a visiting scholar and from the beginning of August in the position of a University Lecturer in petrology.
Beginning in the fall most of my time will, therefore, be spent teaching basic petrology but during the summer I will mostly be concentrating on my book project. Also hoping to finally(!) tie up some loose research project ends before the teaching hassle begins.
So, major gears shifting but I'm excited at the face of all the new challenges...
Friday, June 2, 2017
Tuesday, February 9, 2016
Geology paper on rapakivi zircon
We just got a manuscript accepted in Geology.
The paper (A priori evidence for zircon antecryst entrainment in megacrystic Proterozoic granites) presents a first-order U-Pb and trace element comparison of suspected antecryst zircon populations that are included within the megacrystic rapakivi texture -forming alkali feldspar ovoids to their respective groundmass zircon populations.
We utilized a simple (but also rather tedious) microdrilling approach to extract zircon from within the rapakivi ovoids and were able to show that the populations show dissimilar geochronological and compositional characteristics.
The paper will appear in the March 2016 issue...
Abstract
Entrainment of antecrystic zircon in early saturated main silicate phases has been recognized as a complicating factor in high-precision U-Pb geochronology of Phanerozoic granitic systems, but has not been demonstrated for Precambrian rocks. We report U-Pb ages (secondary ion mass spectrometry) and trace element (laser ablation–inductively coupled plasma–mass spectrometry) compositions of zircon from three main ferroan granite types of the late Paleoproterozoic Wiborg rapakivi granite batholith of southeastern Finland and vicinity. Zircon was extracted from the interior parts of megacrystic (diameters as large as 15 cm) rapakivi-textured alkali feldspar ovoids using a microdrilling technique. Compared to zircon in ovoid groundmass, zircon in the ovoids has higher incompatible element values (e.g., uranium and rare earth elements) and, for two of the three samples examined, slightly older (by ∼1 m.y.) average U-Pb ages. These observations suggest that the ovoid material of the rapakivi granites entrained zircon from earlier magmas that were compositionally different than the final magmatic host of the ovoids. Groundmass zircon implies similar average U-Pb ages for all the studied samples, ca. 1628 Ma; this is regarded as the final crystallization age of the granites. These observations show that it is viable to measure statistically valid age differences between antecrysts and groundmass of Proterozoic granites. Overall, our sampling technique provides enhanced textural control of antecrystic zircon in a wide range of sample materials.
The paper (A priori evidence for zircon antecryst entrainment in megacrystic Proterozoic granites) presents a first-order U-Pb and trace element comparison of suspected antecryst zircon populations that are included within the megacrystic rapakivi texture -forming alkali feldspar ovoids to their respective groundmass zircon populations.
We utilized a simple (but also rather tedious) microdrilling approach to extract zircon from within the rapakivi ovoids and were able to show that the populations show dissimilar geochronological and compositional characteristics.
The paper will appear in the March 2016 issue...
Abstract
Entrainment of antecrystic zircon in early saturated main silicate phases has been recognized as a complicating factor in high-precision U-Pb geochronology of Phanerozoic granitic systems, but has not been demonstrated for Precambrian rocks. We report U-Pb ages (secondary ion mass spectrometry) and trace element (laser ablation–inductively coupled plasma–mass spectrometry) compositions of zircon from three main ferroan granite types of the late Paleoproterozoic Wiborg rapakivi granite batholith of southeastern Finland and vicinity. Zircon was extracted from the interior parts of megacrystic (diameters as large as 15 cm) rapakivi-textured alkali feldspar ovoids using a microdrilling technique. Compared to zircon in ovoid groundmass, zircon in the ovoids has higher incompatible element values (e.g., uranium and rare earth elements) and, for two of the three samples examined, slightly older (by ∼1 m.y.) average U-Pb ages. These observations suggest that the ovoid material of the rapakivi granites entrained zircon from earlier magmas that were compositionally different than the final magmatic host of the ovoids. Groundmass zircon implies similar average U-Pb ages for all the studied samples, ca. 1628 Ma; this is regarded as the final crystallization age of the granites. These observations show that it is viable to measure statistically valid age differences between antecrysts and groundmass of Proterozoic granites. Overall, our sampling technique provides enhanced textural control of antecrystic zircon in a wide range of sample materials.
Thursday, January 21, 2016
NGWM16
Hit the ground running in January with only two weeks to prepare for the Nordic Geological Winter Meeting (NGWM), which were held in Helsinki on 13th to 15th Jan.
I gave a talk on the micro-drilling methods we've been using for zircon sampling and a poster on the geochronological results. Also participated in preparations of three other presentations, which totaled the Wintermeeting at five personal contributions, and chaired a session of Fennoscandian granitic magmatism.
Met a lot of people and had a cool meeting! Didn't have enough time for the social events though, and the poster sessions were organized a bit weirdly in between oral sessions but otherwise all was good.
With that, the quota for scientific meetings is full for the time being... time to concentrate on getting some new material published.
I gave a talk on the micro-drilling methods we've been using for zircon sampling and a poster on the geochronological results. Also participated in preparations of three other presentations, which totaled the Wintermeeting at five personal contributions, and chaired a session of Fennoscandian granitic magmatism.
Met a lot of people and had a cool meeting! Didn't have enough time for the social events though, and the poster sessions were organized a bit weirdly in between oral sessions but otherwise all was good.
With that, the quota for scientific meetings is full for the time being... time to concentrate on getting some new material published.
Monday, December 21, 2015
Pages online
Finally got around to finishing the layouts and most of the content framework on these pages. Some of the features required abit more nerd-out than I expected but I think the end-result looks ok...
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