Results 41 to 50 of about 9,430 (230)
The formation of tephra layers in peatlands: An experimental approach [PDF]
Tephrochronology provides a valuable method of dating peat deposits but results may be compromised if tephra undergoes significant post-depositional movement.
Gehrels, Maria, Payne, Richard
core +1 more source
ABSTRACT The Aso‐3 tephra is one of the most significant widespread marker layers from the Middle to Late Pleistocene, generated by a large caldera‐forming eruption at the Aso volcano in Kyushu, southwestern Japan. Despite its importance, a distal co‐ignimbrite ash correlative has yet to be clearly identified, primarily because although volcanic glass ...
Toshinori Sasaki +6 more
wiley +1 more source
Mortars From Punic and Hellenistic–Roman Solunto: Materials, Formulations, and Technology
ABSTRACT This study presents an archaeometric investigation of 18 hydraulic rendering and bedding mortars from Punic and Hellenistic–Roman Solunto (NW Sicily). The research aimed to characterize raw materials, reconstruct manufacturing sequences, and evaluate technological proficiency through mineralogical and petrochemical analyses.
G. Montana +4 more
wiley +1 more source
The rigorous assessment of volcanic hazards relies on setting contemporary monitoring observations within an accurate, longer-term geological context. Revealing that geological context requires the detailed fieldwork, mapping and laboratory analysis of ...
Chris Satow +4 more
doaj +1 more source
Marine tephrochronology: a personal perspective
This special volume on marine tephrochronology is remarkable, and timely, because it marks a concerted step towards what might be informally termed ‘phase 3’ of a revolution in Quaternary geosciences that began around 40 years ago.
Lowe, David J., David J. Lowe
core +1 more source
The characteristics of settlement of Neanderthals in northern Central Europe during the earlier phases of the Middle Palaeolithic (Marine Isotope Stage 8–6) have been a matter of debate for decades, specifically regarding the population dynamics at such latitudes during the coldest phases. In this paper, we review the known archaeological record of the
Gianpiero Di Maida +5 more
wiley +1 more source
これまでに屈折率の測定されていない大山最下部火山灰と下部火山灰にはさまれるテフラについて,残存する斜方輝石,角閃石,カミングトン閃石の屈折率を測定した.またDMPについては,ごくわずかに斑晶に付着するガラスの屈折率を測定した.最下部火山灰を構成する各テフラは,鉱物組成,斜方輝石および角閃石の屈折率から,それぞれ識別できる.最下部火山灰cpmおよびhpm1のフィッション・トラック年代と,琵琶湖湖底堆積物中の大山火山起源とされるBT44-49火山灰層群の推定堆積年代との対比から,BT44-49火山灰層群の一部は,大山最下部火山灰に対比できる可能性があり,BT44-49火山灰の角閃石および斜方輝石の屈折率が明らかになれば,両地点におけるテフラの対比を検討することが可能と考える.
Furusawa, Akira, Umeda, Koji
openaire +2 more sources
The vegetation history of two mires associated with Holocene dunes near the western Bay of Plenty coast, North Island, New Zealand, is deduced from pollen analysis of two cores.
Wigley, G.N.A. +5 more
core +1 more source
We summarize the current state of knowledge on the age of the Middle Pleistocene ice advances into northern central Europe and provide 25 new single‐grain feldspar luminescence ages of Elsterian and Saalian glacigenic sediments to constrain the age of the ice advances and their tentative correlation with marine isotope stages/substages.
Niklas von Soest +10 more
wiley +1 more source
Volcanic ash (tephra) horizons represent powerful chronological and stratigraphic markers: rapid and widespread deposition allows for correlation of geological records in time and space.
Willem G. M. van der Bilt +8 more
doaj +1 more source

