Cover Image

Cover Image

COVER: Combined bathymetry and root-mean-square (RMS) amplitude response from the tectonically active margin of the Levant Basin (eastern Mediterranean Sea). In the center of the image, a deepwater fan, highlighted by high RMS amplitude values, is cut by an active normal fault. Sedimentary bedforms occur only on the fault footwall, indicating the important control of the topography generated by active tectonics on the flow behavior of turbidity currents. See ‘Active faulting controls bedform development on a deep-water fan’ by Maselli et al., p. 1495–1500.
Table of Contents
Back Matter

All Issues

Email alerts

Early publications alert

New issue alert

RSS Feeds

RSS Feed - Current Issue Only

RSS Feed - Early Publication

Open Issues RSS Feed

Latest
Most Read
Most Cited

Rift propagation across the Tibetan Plateau as a consequence of fluid flow from south to north

Insights into the chemical evolution of sub-arc magmas from the high-pressure electrical conductivity of basaltic and andesitic magmas

Fossil feathers from the Colli Albani volcanic complex (Late Pleistocene, Central Italy) preserved in zeolites

An invasion model for the start of Paleo-Pacific subduction

Unusually fracture-free seafloor in the southern North Atlantic between Newfoundland and Iberia explained through compounding tectonic inheritance since the Paleoproterozoic

Articles

The impact of postdepositional alteration on iron- and molybdenum-based redox proxies

Efficient release of bromine by super-eruptions

Distinguishing volcanic from impact glasses—The case of the Cali glass (Colombia)

The unevenness of the north Iberian crustal root, a snapshot of an elusive stage in margin reactivation

Current and sea level control the demise of shallow carbonate production on a tropical bank (Saya de Malha Bank, Indian Ocean)

Curved orogenic belts, back-arc basins, and obduction as consequences of collision at irregular continental margins

Clear as mud: Clinoform progradation and expanded records of the Paleocene-Eocene Thermal Maximum

Diverse gas composition controls the Moby-Dick gas hydrate system in the Gulf of Mexico

Pulsed volcanism and rapid oceanic deoxygenation during Oceanic Anoxic Event 1a

Spontaneous reheating of crystallizing lava

Zircon (U-Th)/He thermochronology reveals pre-Great Unconformity paleotopography in the Grand Canyon region, USA

Rhabdophane Th-Pb ages indicate reactivation of Mesoarchean structures in west Pilbara Craton during breakup of Greater India and Australia-Antarctica

Early Pleistocene climate-induced erosion of the Alaska Range formed the Nenana Gravel

Cryogenian glaciostatic and eustatic fluctuations and massive Marinoan-related deposition of Fe and Mn in the Urucum District, Brazil

Late Weichselian ice-sheet flow directions in the Russian northern Barents Sea from high-resolution imagery of submarine glacial landforms

A molecular biomarker for end-Permian plant extinction in South China

Active faulting controls bedform development on a deep-water fan

Detrital signals of coastal erosion and fluvial sediment supply during glacio-eustatic sea-level rise, Southern California, USA

River sinuosity describes a continuum between randomness and ordered growth

Near-constant retreat rate of a terrestrial margin of the Laurentide Ice Sheet during the last deglaciation

Tunnel valley infill and genesis revealed by high-resolution 3-D seismic data

Fjord network in Namibia: A snapshot into the dynamics of the late Paleozoic glaciation

Interaction bounding surfaces exposed in migrating transverse aeolian ridges on Mars

Email alerts

RSS Feeds

About GSW

Resources

Explore

Connect

Issues

Articles

Cover Image

Email alerts

RSS Feeds

About GSW

Resources

Explore

Connect

This Feature Is Available To Subscribers Only