Results 21 to 30 of about 285,536 (204)

Facies and paleoenvironmental reconstruction of Early–Middle Miocene deposits in the north-west of the Zagros Basin, Iran

Geologica Carpathica, 2019
Facies analysis and paleoenvironmental reconstruction of the Burdigalian to Langhian Asmari Formation, outcropping in the Khorram Abad Anticline, in the north-west of the Zagros Basin allow us to interpret the carbonate ramp history during the Early ...
Roozpeykar Asghar, Maghfouri-Moghaddam Iraj, Yazdi Mehdi, Yousefi-Yegane Bizhan   +3 more
doaj   +1 more source

High-Frequency Sea-Level Cycle Reconstruction and Vertical Distribution of Carbonate Ramp Shoal Facies Dolomite Reservoir in Gucheng Area, East Tarim Basin

Energies, 2022
During the sedimentary period of the Ordovician Yingshan Formation, the carbonate platform of the Gucheng area in the Tarim basin was characterized by a distally steepened ramp.
Tong Lin, Kedan Zhu, You Zhang, Zihui Feng, Xingping Zheng, Bin Li, Qifan Yi   +6 more
doaj   +1 more source

Geohistorical analysis of the northern part of the Pai-Khoi carbonate parautochthone in Late Devonian–Carboniferous

Литосфера, 2020
Research subject. This article focuses on the geological structure of the northern part of the Pai-Khoi carbonate parautochthone.Materials and methods. The study was based on the data obtained on the key sections of the North-Western Pai-Khoi.
D. A. Gruzdev, A. I. Gerasimova, A. V. Zhuravlev, Ya. A. Vevel   +3 more
doaj   +1 more source

Fault-Block Platform Evolution between Late Cretaceous and Early Miocene along the Margin of the Latium-Abruzzi Carbonate Platform (Southern Prenestini Mountains, Central Apennines, Italy)

Geosciences, 2022
Since the origin of the carbonate platform concept, the reconstruction of the geometry and the evolution of the margin has been an intriguing topic. The Latium-Abruzzi platform is one of the largest shallow water domains of the Central Apennines, however,
Marco Brandano, Irene Cornacchia, Rita Catanzariti   +2 more
doaj   +1 more source

Facies and depositional settings of the Middle Eocene-Oligocene carbonates in Kutch

Geodinamica Acta, 2018
Middle Eocene Fulra Limestone and Oligocene Maniyara Fort Formation represent platform carbonate deposits of Kutch at the north-western margin of India.
Santanu Banerjee, Sonal Khanolkar, Pratul Kumar Saraswati   +2 more
doaj   +1 more source

Effect of ramp bicycle exercise on exhaled carbon monoxide in humans

The Journal of Physiological Sciences, 2011
The effect of exercise on the increase of exhaled CO in smokers compared to non-smokers has not been clarified yet. In this study we compared the dynamics of exhaled CO before, during and after exercise between smokers and non-smokers. A group of 8 smokers and a group of 8 non-smokers underwent a bicycle exercise in a ramp fashion to near maximum ...
Yoshifumi, Yasuda, Tomonori, Ito, Miharu, Miyamura, Masatsugu, Niwayama   +3 more
openaire   +2 more sources

Mangarara Formation: exhumed remnants of a middle Miocene, temperate carbonate, submarine channel-fan system on the eastern margin of Taranaki Basin, New Zealand [PDF]

, 2009
The middle Miocene Mangarara Formation is a thin (1–60 m), laterally discontinuous unit of moderately to highly calcareous (40–90%) facies of sandy to pure limestone, bioclastic sandstone, and conglomerate that crops out in a few valleys in North ...
Peter J.J. Kamp, Nelson, Campbell S., Ángel Puga‐Bernabéu, Adam J. Vonk, Campbell S. Nelson, Vonk, Adam J., Kamp, Peter J.J., Puga-Bernabéu, Ángel   +7 more
core   +1 more source

Response of carbonate factories to late Paleozoic climate change: a case study from the Yanduhe section, Hubei Province, South China

Frontiers in Marine Science
The carbonate factory concept was proposed to understand the spatial dynamics and processes involved in carbonate production, which was heavily influenced by climate change.
Zihang Huang, Xuefei Yi, Yunfei Huang, Li Tian, Kui Wu, Mengfan Li   +5 more
doaj   +1 more source

Discriminating cool-water from warm-water carbonates and their diagenetic environments using element geochemistry: the Oligocene Tikorangi Formation (Taranaki Basin) and the dolomite effect [PDF]

, 2004
Fields portrayed within bivariate element plots have been used to distinguish between carbonates formed in warm- (tropical) water and cool- (temperate) water depositional settings.
Nelson, Campbell S., Hood, Steven D., Campbell S. Nelson, Kamp, Peter J.J., Steven D. Hood, Peter J. J. Kamp   +5 more
core   +1 more source

The Paleogene Carbonate Banks of the Zagros Foreland Basin’s Forebulge, Northern Iraq: Stratigraphic Architectures and Facies Associations

Iraqi Geological Journal
The Paleogene sequence of the Zagros foreland basin of NE Arabiais punctuated by a linear chain of carbonate bank-ramp associations. These carbonate banks had developed over the NW-SE trending basin forebulge.
Basim Al-Qayim
doaj   +1 more source