Results 81 to 90 of about 11,926 (218)
The Depositional Record, Volume 11, Issue 1, Page 121-146, February 2025.Miocene karstic Lake Sinj. A prograding carbonate bench on a gently inclined lake margin showing shallowing upwards tendency, and closing of the lake. Abstract In the Early to Middle Miocene, the post‐orogenic intramontane lacustrine Sinj Basin that belonged to the Dinarides Lake System evolved in the area of the External Dinarides.
Alan Vranjković +9 more
wiley +1 more source
Geologija, 2007 After a short-lived »ban«, the Quaternary has again been formalized as a chronostratigraphic unit, consisting of the Pleistocene and the Holocene.
Miloš Bavec
doaj
Journal of Maps, 2018 This paper is the first integrated account of the sedimentology, stratigraphy, and vertebrate paleontology for the marine strata of the Chilcatay Formation exposed at Ullujaya, Pisco basin (southern Peru).
C. Di Celma +13 more
doaj +1 more source
Role of tidal range and coastline morphology on the evolution of two macrotidal sand spits
The Depositional Record, Volume 11, Issue 1, Page 311-327, February 2025.Based on historical map and stratigraphic data, the construction dynamics of two sandspits, respectively, subject to macrotidal and hypertidal range (6.5 m vs. 14 m), and that both appeared at the end of the 17th century, are compared. The hypertidal spit developed fast, between 1650 and 1750 CE, with a dominant seaward direction while the macrotidal ...
Bernadette Tessier +6 more
wiley +1 more source
THE GELASIAN STAGE: A PROPOSAL OF A NEW CHRONOSTRATIGRAPHIC UNIT OF THE PLIOCENE SERIES
Rivista Italiana di Paleontologia e Stratigrafia, 2017 A new Stage, the Gelasian, is proposed as the third upper subdivision of the Pliocene Series. The GSSP of the base of the Gelasian Stage and of the Middle Pliocene-Upper Pliocene boundary is coincident with a "sapropel" level which outcrops in the Monte ...
DOMENICO RIO +2 more
doaj +1 more source
The Anthropocene concept as a wake-up call for reforming democracy [PDF]
, 2018 Human activity has reshaped all parts of the Earth system. For this reason, a vast majority of geologists at the 35th International Geological Congress in Cape Town (September 2016) spoke out in favor of changing the classification of geological epochs ...
Tremmel, Jörg
core +1 more source
The Depositional Record, Volume 11, Issue 1, Page 328-353, February 2025.Four different types of elementary sequences (condensed, catch‐down, catch‐up and give‐up) were recognised and interpreted in terms of relative sea‐level changes to reconstruct the relative sea‐level curve of the entire succession. The envelope of the reconstructed relative sea‐level curve was used to represent the long‐term accommodation change on the
Luigi Spalluto +3 more
wiley +1 more source
High resolution carbon isotope stratigraphy of the basal Silurian stratotype (Dob's Linn, Scotland) and its global correlation [PDF]
, 1997 Since its designation as the Global Stratotype Section and Point (GSSP) for the base of the Silurian System, the choice of Dob's Linn, Southern Scotland, has received criticism due to the difficulties of relating its well constrained graptolite ...
Brenchley, P.J. +3 more
core +1 more source
Punctuated aggradation and flow criticality in deep water channel systems
The Depositional Record, Volume 11, Issue 1, Page 354-372, February 2025.Sinuous deepwater channels may form meander belts or aggrading systems, and may alternate between the two states repeatedly. We invoke two‐layer subcritical flow to explain their river‐like behaviour, and suggest that a switch from subcritical to supercritical flow may be responsible for the change in behaviour from meandering to aggrading.
Ben Kneller, Victoria Valdez Buso
wiley +1 more source
Ammonites and stratigraphy of a Lower Bajocian (Middle Jurassic) section in Sierra Chacaico (Neuquén Basin, Argentina) [PDF]
, 2012 A Lower Bajocian section from southern Neuquén Basin (Argentina), with 3 faunal horizons (sphaeroceroides, submicrostoma and giebeli horizons) in the Singularis and Giebeli zones, is described.
Dietze, Volker +3 more
core +2 more sources