Itrax μ‐XRF core scanning for rapid tephrostratigraphic analysis: a case study from the Auckland Volcanic Field maar lakes

2019 ◽  
Vol 35 (1-2) ◽  
pp. 54-65 ◽  
Author(s):  
Leonie Peti ◽  
Patricia S. Gadd ◽  
Jenni L. Hopkins ◽  
Paul C. Augustinus
2015 ◽  
Vol 123 ◽  
pp. 58-75 ◽  
Author(s):  
Jenni L. Hopkins ◽  
Marc-Alban Millet ◽  
Christian Timm ◽  
Colin J.N. Wilson ◽  
Graham S. Leonard ◽  
...  

2013 ◽  
Vol 54 (10) ◽  
pp. 2125-2153 ◽  
Author(s):  
Lucy E. McGee ◽  
Ian E. M. Smith ◽  
Marc-Alban Millet ◽  
Heather K. Handley ◽  
Jan M. Lindsay

2018 ◽  
Author(s):  
Megan M. Ferguson ◽  
◽  
Michael C. Rowe ◽  
Manuela Tost ◽  
Karoly Nemeth

1994 ◽  
Vol 37 (2) ◽  
pp. 143-153 ◽  
Author(s):  
R. M. Briggs ◽  
T. Okada ◽  
T. Itaya ◽  
H. Shibuya ◽  
I. E. M. Smith

2021 ◽  
Vol 29 ◽  
pp. 19-37
Author(s):  
Benjamin Läuchli ◽  
Paul Christian Augustinus ◽  
Leonie Peti ◽  
Jenni Louise Hopkins

Abstract. The accurate and precise reconstruction of Quaternary climate as well as the events that punctuate it is an important driver of the study of lake sediment archives. However, until recently lake sediment-based palaeoclimate reconstructions have largely concentrated on Northern Hemisphere lake sequences due to a scarcity of continuous and high-resolution lake sediment sequences from the Southern Hemisphere, especially from the southern mid-latitudes. In this context, the deep maar lakes of the Auckland Volcanic Field of northern New Zealand are significant as several contain continuous and well-laminated sediment sequences. Onepoto Basin potentially contains the longest temporal lake sediment record from the Auckland Volcanic Field (AVF), spanning from Marine Isotope Stage 6e (MIS 6e) to the early Holocene when lacustrine sedimentation was terminated by marine breach of the south-western crater tuff ring associated with post-glacial sea-level rise. The Onepoto record consists of two new, overlapping cores spanning ca. 73 m combined with archive material in a complete composite stratigraphy. Tephrochronology and 14C dating provide the fundamental chronological framework for the core, with magnetic relative palaeo-intensity variability downcore, and meteoric 10Be influx into the palaeolake to refine the chronology. The µ-XRF (micro X-ray fluorescence) downcore variability for the entirety of the lake sediment sequence has been established with measurement of a range of proxies for climate currently underway. This work will produce the first continuous record of the last 200 kyr of palaeoclimate from northern New Zealand to date.


2020 ◽  
Vol 177 (5) ◽  
pp. 1039-1056
Author(s):  
Thomas B. Phillips ◽  
Craig Magee

Intraplate volcanism is widely distributed across the continents, but the controls on the 3D geometry and longevity of individual volcanic systems remain poorly understood. Geophysical data provide insights into magma plumbing systems, but, as a result of the relatively low resolution of these techniques, it is difficult to evaluate how magma transits highly heterogeneous continental interiors. We use borehole-constrained 2D seismic reflection data to characterize the 3D geometry of the Tuatara Volcanic Field located offshore New Zealand's South Island and investigate its relationship with the pre-existing structure. This c. 270 km2 field is dominated by a dome-shaped lava edifice, surrounded and overlain by c. 69 volcanoes and >70 sills emplaced over 40 myr from the Late Cretaceous to Early Eocene (c. 85–45 Ma). The Tuatara Volcanic Field is located above a basement terrane boundary represented by the Livingstone Fault; the recently active Auckland Volcanic Field is similarly located along-strike on North Island. We suggest that the Livingstone Fault controlled the location of the Tuatara Volcanic Field by producing relief at the base of the lithosphere, thereby focussing lithospheric detachment over c. 40 myr, and provided a pathway that facilitated the ascent of magma. We highlight how observations from ancient intraplate volcanic systems may inform our understanding of active intraplate volcanic systems, including the Auckland Volcanic Field.Supplementary material: Interpreted seismic section showing well control on stratigraphic interpretation is available at https://doi.org/10.6084/m9.figshare.c.5004464


Lithos ◽  
2012 ◽  
Vol 155 ◽  
pp. 360-374 ◽  
Author(s):  
Lucy E. McGee ◽  
Marc-Alban Millet ◽  
Ian E.M. Smith ◽  
Károly Németh ◽  
Jan M. Lindsay

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