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Oxygen isotope values from biogenic apatite (conodont elements and fish teeth...
Recovery from the end-Permian mass extinction is frequently described as delayed, with complex ecological communities typically not found in the fossil record until the Middle... -
Tab. 1+2: C14-dates cf the older and younger emergence periods
In the neighbourhood of Oobloyah Bay various phenomena ean be eneountered whieh point to a ularge-seale uplift of shorelines, i.e. to an emergence of 200 m. Delta terraces,... -
Table D.14: Microprobe analyses of garnets from sample 2119
Number of ions on the basis of 24 O; oxides given in weight percentage -
Table C.18: Microprobe analysis of garnets from samples no. 2168 and 2181
Number of ions on the basis of 24 O; oxides given in weight percentage -
Table C.17: Microprobe analysis of garnets from sample no. 1563
Number of ions on the basis of 24 O; oxides given in weight percentage -
Table C.15+16: Microprobe analysis of garnets from sample no. 1562
Number of ions on the basis of 24 O; oxides given in weight percentage -
X-ray fluorescence data from Contessa Road (Italy), Paleocene-Eocene Thermal ...
The Paleocene-Eocene Thermal Maximum (PETM) is the most studied global warming event of a series of Paleocene-Eocene carbon cycle perturbations called hyperthermals. PETM... -
U-Pb age analyses on zircon grains from Mount Lawson Formation bentonites (El...
LA-ICP-MS analyses on zircon grains from Mount Lawson Formation bentonites (Ellesmere Island). Analyses listed from lowest to highest 206Pb/238U age for <1000 Ma and lowest... -
U-Pb age analyses on zircon grains from Basilika Formation bentonites (Bjørnd...
LA-ICP-MS analyses on zircon grains from Basilika Formation bentonites (Bjørndalen area). Analyses listed from lowest to highest 206Pb/238U age for <1000 Ma and lowest to... -
Major and trace element composition of whole-rock samples from the Basilika F...
This dataset has no description
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Sm-Nd isotope data of whole-rock bentonite samples from Svalbard (including C...
Initial EpsilonNd (EpsilonNd(t)) calculated with 60 Ma for Basilika Fm. bentonites and Lawson-ash 1 and 54 Ma for Lawson ash 2. -
Sm-Nd isotope data of bentonite samples (<2 µm fractions) from Svalbard and E...
Initial EpsilonNd (EpsilonNd(t)) calculated with 60 Ma for Basilika Formation bentonites and Lawson-ash 1 and 54 Ma for Lawson ash 2. -
Chemical composition of Basilika Formation (Bjørndalen area) and Mount Lawson...
This dataset has no description
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Major and trace element composition of whole-rock samples from the Basilika F...
This dataset has no description
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Table 4. Radiocarbon age determinations of samples collected around Loon Lake
This dataset has no description
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Table 2. AIle/Ile ratios in the total hydrolysate (HYD) and free fraction of ...
This dataset has no description
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Paleontological and sedimentological investigations of a sediment profile fro...
The Kap Mackenzie area on the outer coast of northeast Greenland was glaciated during the last glacial stage, and pre-Holocene shell material was brought to the area. Dating of... -
(Table 1) Mean grain sizes and standard deviations of gas hydrate samples
Methane hydrates are present in marine seep systems and occur within the gas hydrate stability zone. Very little is known about their crystallite sizes and size distributions... -
Tab. 1: Proportion of glacial quartz grains contained in the deposits
The Yari-Hotaka Mountain Range is one of the most famous formerly-glaciated areas of Japan. Many glacial landforms remain in three neighbouring U-shaped valleys, named Yarisawa,... -
AMS and EBSD maps of rock salt - lamprophyre dyke contact zone, Loule diapir,...
A rock salt-lamprophyre dyke contact zone (sub-vertical, NE-SW strike) was investigated for its petrographic, mechanic and physical properties by means of anisotropy of magnetic...
