Results 161 to 170 of about 79,295 (351)

Plio-Pleistocene in the Toikanbetsu Tectonic Basin, Northern Hokkaido. Sedimentary facies and pollen stratigraphy.

, 1993
Takao Oka, Yaeko Igarashi
openalex   +2 more sources

Automatic Identification of Sedimentary Facies Based on a Support Vector Machine in the Aryskum Graben, Kazakhstan [PDF]

, 2019
Xiao Ai, Hongyu Wang, Baitao Sun
openalex   +1 more source

Polygonal tepee structures of Arabia

The Depositional Record, Volume 12, Issue 1, February 2026.
Tepee structures on Sheybarah Island form polygonal microbial cemented crusts in the intertidal. Radiocarbon dating suggests they formed in the Holocene and reflect minor sea‐level changes, highlighting their value as palaeoenvironmental indicators. Satellite surveys identified 126 polygonal features, including coral reefs that may have developed on ...
Pauline Falkenberg, Sarima Vahrenkamp, Elisa Garuglieri, Alexander Petrovic, Kai Hachmann, Viswasanthi Chandra, Volker C. Vahrenkamp   +6 more
wiley   +1 more source

Sedimentary environments of the lower Miocene Nojima Group, NW Kyushu, inferred from sedimentary facies and total organic carbon and total sulfur concentrations.

, 2003
Junko Komatsubara, Yoshihisa Hiroki, Ryo Matsumoto   +2 more
openalex   +2 more sources

Sedimentary facies, depositional environments and palaeogeographic

, 2007
The Denizli Basin (southwestern Anatolia, Turkey) contains a record of environmental changes dating since the Early Miocene. Detailed facies analysis of the Neogene formations in this half-graben enables us to document successive depositional regimes and palaeogeographic settings.
Alcicek, H, Varol, B, Ozkul, M
openaire   +2 more sources

Orbital and eustatic control of basin hydrology during the first stage of the Messinian Salinity Crisis

The Depositional Record, Volume 12, Issue 1, February 2026.
The paleo‐hydrology of the Sorbas Basin (SE Spain) and the wider Mediterranean region during the deposition of the Primary Lower Gypsum (PLG) stage of the Messinian Salinity Crisis, from ~5.97 to ~5.60 Ma, was affected by tectonics, precession‐forced climate oscillations, and eustatic sea‐level change.
Fernando Gázquez, Nicholas P. Evans, Thomas K. Bauska, Harold J. Bradbury, Alexandra V. Turchyn, María del Carmen Barroso, Alexander M. Piotrowski, José María Calaforra, David A. Hodell   +8 more
wiley   +1 more source

Seismic prediction of shale oil lithofacies associations based on sedimentary facies patterns: A case study of the shahejie formation in the Huanghekou Sag. [PDF]

PLoS One
Zhao H, Wang H, Wang G, Wan L.
europepmc   +1 more source

Characteristics of Core Sedimentary Facies at the Ulleung Basin in the East Sea of Korea [PDF]

, 2011
Byoung-Kwan Lee, Su-Woong Lee, Hong‐Tae Kim, Seok-Yun Kim   +3 more
openalex   +1 more source

Deciphering depositional controls and evolution of a lacustrine supradetachment basin through facies analysis: Gördes Basin, Western Türkiye

The Depositional Record, Volume 12, Issue 1, February 2026.
The lacustrine Gördes Supradetachment Basin was developed along the Simav detachment fault during postorogenic extension in the north of the Menderes Massif in western Anatolia. The basin‐fill succession is represented by alluvial fan, Gilbert‐type delta, shoal‐water delta, foreshore, shoreface, offshore‐transition and peat‐forming mire deposits.
Ayhan Ilgar, Alper Bozkurt, Tolga Esirtgen, Ali Ergen, Ercan Tuncay, Sema Çobankaya   +5 more
wiley   +1 more source

Heterolytic tide-dominated sedimentary facies and depositional environment: An Example from the Boka Bil formation, Sitapahar anticline, Bangladesh. [PDF]

Heliyon
Ali S, Siddiqui NA, Haque AE, Ahmed N, El-Ghali MAK, Arafath MY, Rahman M, Roy MK, Rashid A.   +8 more
europepmc   +1 more source