Results 31 to 40 of about 5,823,618 (83)

Seismic data reveal eastern Black Sea Basin structure [PDF]

open access: yes, 2005
Rifted continental margins are formed by progressive extension of the lithosphere. The development of these margins plays an integral role in the plate tectonic cycle, and an understanding of the extensional process underpins much hydrocarbon ...
Price, A.   +43 more
core   +1 more source

Fluorescence as a tracer of the susceptibility of dissolved organic matter to photodegradation in the Arctic Ocean

open access: yesLimnology and Oceanography, Volume 70, Issue 8, Page 2299-2314, August 2025.
Abstract The Arctic Ocean exports a large amount of terrestrial dissolved organic matter (DOM) to the Nordic seas. With climate change, the supply of terrestrial DOM from the Arctic Ocean will increase while less sea ice might lead to an increased loss of terrestrial DOM due to photodegradation.
Urban J. Wünsch   +5 more
wiley   +1 more source

Geothermics of the Malay basin, offshore Malaysm [PDF]

open access: yes, 1993
A review of the temperature, thermal conductivity and heat flow data of the Malay Basin has been carried out by analysing data from fifty nine exploration wells.
Yusoff, Wan Ismail Wan
core  

The Role of the St. Anna Trough in Atlantic Water Transport Into the Arctic Ocean: A Novel Radiogenic Isotope Assessment Using Iodine, Uranium, and Neodymium

open access: yesJournal of Geophysical Research: Oceans, Volume 130, Issue 4, April 2025.
Abstract The St. Anna Trough (SAT) plays a critical role in Arctic Ocean circulation by facilitating heat and water mass exchange, influencing sea‐ice melt and thermohaline dynamics. However, ocean circulation in this key region remains understudied compared to other parts of the Arctic.
H. Pérez‐Tribouillier   +9 more
wiley   +1 more source

Lithology and provenance of late Eocene - Oligocene sediments in eastern Taranaki Basin margin and implications for paleogeography [PDF]

open access: yes, 2009
The latest Eocene and Oligocene was a time of marked paleoenvironmental change in Taranaki Basin, involving a transition from the accumulation of coal measures and inner shelf deposits to the development of upper bathyal environments. Up until the end of
Hopcroft, Bradley Scott
core  

Petrogenesis of diachronous mixed siliciclastic-carbonate megafacies in the cool-water Oligocene Tikorangi Formation, Taranaki Basin, New Zealand [PDF]

open access: yes, 2003
The Oligocene (Whaingaroan-Waitakian) Tikorangi Formation is a totally subsurface, lithostratigraphically complex, mixed siliciclastic-limestone-rich sequence forming an important fracture reservoir within Taranaki Basin, New Zealand.
Nelson, Campbell S.   +5 more
core   +1 more source

The Skiddaw Group of Cumbria : early Ordovician Turbidite sedimentation and provenance on an evolving microcontinental margin. [PDF]

open access: yes, 1992
During the Early Palaeozoic, the southern British Isles were part of a microcontinent Eastern Avalonia. In the early Ordovician Eastern Avalonia was close to the continent of Gondwana. in high southern latitudes.
Moore, Richard Maurice
core   +5 more sources

Elemental and Li Isotopic Investigation of a Proglacial River System: Insights to Modern Chemical Weathering Processes

open access: yesJournal of Geophysical Research: Earth Surface, Volume 130, Issue 4, April 2025.
Abstract Dissolved and suspended sediment samples were collected from the 121 km‐long proglacial Matanuska River and five associated tributaries in Southcentral Alaska (USA), in July 2019. Li elemental and isotopic (δ7Li) composition of dissolved load from proglacial river water samples and XRD analyses of the accompanying suspended sediments were ...
Venkata Sailaja Pappala   +2 more
wiley   +1 more source

Tertiary tectonics and sedimentation history of the Sarawak basin, east Malaysia [PDF]

open access: yes, 1996
A seismic stratigraphic study of the regional lines for the offshore Sarawak area was undertaken with the aim of understanding the tectonics and sedimentation history of the hydrocarbon prolific Sarawak Basin.
Zin, Ismail Che Mat
core  

A fluid flow perspective on the diagenesis of Te Aute limestones [PDF]

open access: yes, 2003
Pliocene cool-water, bioclastic Te Aute limestones in East Coast Basin, New Zealand, accumulated either in shelfal shoal areas or about structurally shallow growth fold structures in the tectonically active accretionary forearc prism.
Nelson, Campbell S.   +8 more
core   +1 more source

Home - About - Disclaimer - Privacy