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Investigation of Palaeocene Eocene Thermal Maximum Impacts on Larger Benthic ...
The Palaeocene Eocene Thermal Maximum (PETM) is a well-studied event globally, yet it has received limited attention in the central eastern Tethys region. This study focuses on... -
Table 7.3: Modal compositions of samples from shear zones within the O.-v.-Gr...
In thinsection 1588-1B modal estimations only refer to the shear plane, not to the whole thinsection as it is a c. 1.0 cm wide sharply defined layer in light-grey anorthosite;... -
Table 7.2: Modal compositions of samples taken from the O.-v.-Gruber anorthos...
composition given in volume % -
Table 6.4: Modal compositions of different younger plutonic rocks that intrud...
composition given in volume % -
Table 6.3: Modal compositions of light varieties of gneiss and migmatite samp...
composition given in volume % -
Table 6.2: Modal compositions of dark varieties of gneissic samples from the ...
composition given in volume % -
Volcanic glass shard concentration in the size fraction between 45 and 100 mi...
Concentrations of volcanic glass shards of the sediment size fraction between 45 - 100 micrometer of sediments of core DP30PC (southeastern Gulf of Taranto) have been determined... -
Heavy minerals from sediment core POS514_40-11
In order to study influence of changing oceanographic setting and climate on carbon burial efficiency and provenance of detrital component a sedimentary core (POS514-40-11GC)... -
Heavy minerals of sediment cores PS69/849-1 and PS69/849-2
This dataset has no description
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(Table 3) Light-minerals for DSDP Leg 67 Holes
This dataset has no description
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(Table 3) Clay minerals in DSDP Leg 67 Holes
<1 indicate that very small percentages were detected. Samples in which kaolinite was identified by destruction of the X-ray peak upon heating to 500°C; partial destruction...
