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Pliocene-Pleistocene stable isotope record of ODP Site 107-653
Planktonic foraminiferal oxygen and carbon isotope analyses from Tyrrhenian Sea Ocean Drilling Program (ODP) Site 653 provide a continuous record of the Pliocene-Pleistocene... -
Benthic foraminifera and ostracoda in ODP Hole 107-650A
Twenty-three sediment intervals from top of Site 650 down to 510 m below seafloor have been studied. Their thicknesses vary between 0.25 m and about 40 m. The studied deposits... -
Geochemistry of Messinian sediments of the Sardinian margin
Brightly colored mudstones within Messinian (late Miocene) and lower Pliocene successions were cored beneath the upper and lower slopes of the Sardinian continental margin of... -
Volcanoclastic sediments in the Tyrrhenian Basin
The results of lithologic, petrographic, grain-size, and chemical studies of volcaniclastic sediments recovered during Leg 107 of the Ocean Drilling Program show that a variety... -
Oxygen and carbon isotope stratigraphy of ODP Holes 107-653A and 107-654A
Stable isotope analysis of two species (or groups of species) of planktonic foraminifers: Globigerinoides ruber (or G. obliquus and G. obliquus extremus) and Globigerina... -
Magnetostratigraphy of ODP Leg 107 holes
Apart from Site 650, core disturbance due to rotary drilling severely compromised the quality of the magnetostratigraphic data obtained from Leg 107 sediments. The correlation... -
Geochemistry of sediments from the Tyrrhenian Sea
At Holes 650A and 651 A, set respectively in the Marsili Basin and the Vavilov Basin, Pleistocene sediments (turbiditic inputs interbedded with essentially hemipelagic... -
Messinian and pre-Messinian sediments of ODP Holes 107-652A and 107-654A
Sedimentology, mineralogy, and petrology of the pre-Pliocene sediments drilled at ODP Sites 652 and 654 in the Tyrrhenian Sea (Leg 107) have been studied with emphasis on the... -
Grain size distribution and clay mineralogy of upper Miocene sediments of ODP...
The upper Miocene sedimentary sequence of Site 652, located on the lower continental margin of eastern Sardinia, was cored and logged during Ocean Drilling Program (ODP) Leg... -
Composition of Messinian sediments from the Tyrrhenian Sea
The data base for this study is represented by essentially nonevaporitic Messinian sediments recovered at ODP Sites 654, 653, 652, and 656 along the eastern Sardinian margin,... -
Stable isotope composition of carbonates in the Tyrrhenian Sea
The Messinian evaporitic succession recovered at ODP Sites 652, 653, and 654 in the Tyrrhenian Sea was generated under various environmental conditions which ranged from... -
Mineralogy and geochemistry of latest Miocene deposits in the Tyrrhenian Sea
Late Miocene sediments from ODP Sites 652 and 654, drilled on the Sardinian margin in the Western Tyrrhenian Sea, are investigated through mineralogical, micromorphological,... -
Basal dolomitic sediments ofthe Tyrrhenian Sea
Basal dolomitic sediments were recovered at three drill sites in the Tyrrhenian Sea during Ocean Drilling Program (ODP) Leg 107 (Sites 650, 651, and 655). These sediments... -
Geochemistry of basal dolomitic and Fe-Mn sediments from the Tyrrhenian Sea
In the Tyrrhenian Sea (Western Mediterranean), unusual reddish, soft to lithified, dolomitic sediments up to 45 m thick overlie igneous crust at the base of thick... -
Magnetic properties and paleomagnetism of basalts from ODP Leg 107 basalts
The basalts recovered at Holes 651A and 655B appear to carry a single component remanent magnetization, which is generally of reversed polarity. These magnetizations are... -
Petrology and geochemistry of basalts from the Vavilov Basin
During ODP Leg 107, two holes were drilled in the basement of Vavilov Basin, a central oceanic area of the Tyrrhenian sea. Hole 655B is located near the Gortani ridge in... -
Geochemistry and mineralogy of ODP Leg 107 basalts
During ODP Leg 107, the basement of the Tyrrhenian Sea was drilled at Site 650, located in the Marsili basin, and at Sites 651 and 655, both located in the Vavilov basin. In... -
Chemistry of peridotites from ODP Hole 107-651A
Hole 651 A, drilled during ODP leg 107 in the Tyrrhenian Sea, bottomed in a 30-m-thick section of serpentinized peridotite. Site 651 was drilled on the eastern flank of a... -
Calcareous nannofossils of ODP Leg 107 holes
This paper summarizes the nannoplankton biostratigraphy and the paleoenvironmental interpretations obtained from Leg 107 in the Tyrrhenian Sea. Marine sediments are ranging in... -
Planktonic foraminifera of ODP Hole 107-654A
The late Miocene sediments of the Tyrrhenian ODP Site 654 encompass a deepening sequence which begins with glauconite shallow water sands followed by a rapid transition to deep...