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Morphodynamics of rivers strongly affected by monsoon precipitation: review of depositional style and forcing factors
P Plink-Björklund - Sedimentary Geology, 2015 - Elsevier
Rivers that receive significant amounts of their surface water supply from monsoon
precipitation characteristically experience seasonal floods, and display seasonally highly …
precipitation characteristically experience seasonal floods, and display seasonally highly …
Zircon U‐Pb ages and Hf isotopes of the Askot klippe, Kumaun, northwest India: Implications for Paleoproterozoic tectonics, basin evolution and associated …
Throughout the Himalayan thrust belt, klippen of questionable tectonostratigraphic affinity
occur atop Lesser Himalayan rocks. Integrated U‐Pb ages, Hf isotopic, and whole rock trace …
occur atop Lesser Himalayan rocks. Integrated U‐Pb ages, Hf isotopic, and whole rock trace …
Soft-sediment deformation structures in Cambrian siliciclastic and carbonate storm deposits (Shandong Province, China): Differential liquefaction and fluidization …
This paper focuses on soft-sediment deformation structures (SSDS) in both siliciclastic and
carbonate storm deposits of the Cambrian Mantou and Chaomidian formations (Shandong …
carbonate storm deposits of the Cambrian Mantou and Chaomidian formations (Shandong …
Early Cretaceous slumps and turbidites with peculiar soft-sediment deformation structures on Lingshan Island (Qingdao, China) indicating a tensional tectonic regime
R Yang, AJT van Loon - Journal of Asian Earth Sciences, 2016 - Elsevier
Abstract Some sections on Lingshan Island, in the Yellow Sea, close to the city of Qingdao,
show the Early Cretaceous Lingshandao Formation. The exposed succession consists …
show the Early Cretaceous Lingshandao Formation. The exposed succession consists …
Redefining the tectonostratigraphic and structural architecture of the Almora klippe and the Ramgarh–Munsiari thrust sheet in NW India
We integrate U–Pb zircon geochronology and ɛ Nd (0) values with field map** to
determine which tectonostratigraphic units are represented to the north, south and within the …
determine which tectonostratigraphic units are represented to the north, south and within the …
Genesis and implication of soft-sediment deformation structures in high-energy fluvial deposits of the Alaknanda Valley, Garhwal Himalaya, India
Valley-fill terraces and fluvio-lacustrine sediment successions were investigated for the
nature and type of soft-sediment deformation structures (SSDS) in the Alaknanda Valley of …
nature and type of soft-sediment deformation structures (SSDS) in the Alaknanda Valley of …
Provenance and sedimentation age of the Proterozoic clastic succession of the Garhwal‐Kumaon Lesser Himalaya, NW‐India: Clues from U–Pb zircon and Sr–Nd …
The paper presents data on the U–Pb chronology of detrital zircon grains and radiogenic
isotopic composition (87Sr/86Sr, ɛNd) from the Proterozoic clastic successions of the …
isotopic composition (87Sr/86Sr, ɛNd) from the Proterozoic clastic successions of the …
Pre‐Vegetation Mixed (Wave‐Tide) Energy Trangressive Nearshore Sedimentation: Evidence From the Proterozoic Passive Margin Sequence of NW Himalaya, India
S Saha - Geological Journal, 2024 - Wiley Online Library
The coupled evolution of the Earth's atmosphere–biosphere system through time has
caused irreversible changes in the geodynamics as well as surface processes and …
caused irreversible changes in the geodynamics as well as surface processes and …
Core evidence of paleoseismic events in Paleogene deposits of the Shulu Sag in the Bohai Bay Basin, east China, and their petroleum geologic significance
Abstract The Shulu Sag, located in the southwestern corner of the Jizhong Depression,
Bohai Bay Basin of east China, is a NE–SW trending, elongate Cenozoic half-graben basin …
Bohai Bay Basin of east China, is a NE–SW trending, elongate Cenozoic half-graben basin …
Seismic origin of the soft‐sediment deformation structures in the upper Palaeo‐Mesoproterozoic Semri Group, Vindhyan Supergroup, Central India
Soft‐sediment deformation (SSD) structures are the syn‐sedimentary structures that can
form by seismic as well as non‐seismic processes. The SSD structures commonly occur in …
form by seismic as well as non‐seismic processes. The SSD structures commonly occur in …