Eastern Turkish high plateau as a small Turkic-type orogen: Implications for post-collisional crust-forming processes in Turkic-type orogens
Post-collisional magmatism may be generated by extensive crustal melting in Tibet-type
collisional environments or by falling out of slabs from under giant subduction–accretion …
collisional environments or by falling out of slabs from under giant subduction–accretion …
Microbialites and global environmental change across the Permian–Triassic boundary: a synthesis
Abstract Permian–Triassic boundary microbialites (PTBMs) are thin (0.05–15 m) carbonates
formed after the end‐Permian mass extinction. They comprise Renalcis‐group …
formed after the end‐Permian mass extinction. They comprise Renalcis‐group …
[PDF][PDF] The global stratotype section and point (GSSP) of the Permian-Triassic boundary
Y Hongfu, Z Kexin, T **nan… - Episodes …, 2001 - indianjournalofentrepreneurship …
Figure 3 Litho-and biostratigraphic column of PTB strata of Meishan section D. l.-m. Z.
Hindeodus latidentatus-Clarkina meishanensis Zone, SB sequence surface, LB …
Hindeodus latidentatus-Clarkina meishanensis Zone, SB sequence surface, LB …
A new model for the late Palaeozoic—Mesozoic tectonic evolution of Iran and implications for Oman
AMC Şengör - Geological Society, London, Special Publications, 1990 - lyellcollection.org
It has been suggested that in a number of places such as Greece, Turkey, the Central
Pamirs, and Thailand Neo-Tethys may have opened as a back-arc basin above a Palaeo …
Pamirs, and Thailand Neo-Tethys may have opened as a back-arc basin above a Palaeo …
Tethyan margins in space and time
Rifting processes, leading to sea-floor spreading, are characterized by a sequence of
events: transtensive phase of extension with syn-rift volcanism; simple shear extension …
events: transtensive phase of extension with syn-rift volcanism; simple shear extension …
[HTML][HTML] Opening of the Neo-Tethys Ocean and the Pangea B to Pangea A transformation during the Permian
We studied the stratigraphy, composition, and paleomagnetic properties of lateritic
weathering profiles of Permian age from northern Iran and western Karakoram, Pakistan. A …
weathering profiles of Permian age from northern Iran and western Karakoram, Pakistan. A …
Permian-Triassic of the Tethys: Carbon isotope studies
A Baud, M Magaritz, WT Holser - Geologische Rundschau, 1989 - Springer
Profiles of carbon isotopes were studied in marine limestones of Late Permian and Early
Triassic age of the Tethyan region from 20 sections in Yugoslavia, Greece, Turkey …
Triassic age of the Tethyan region from 20 sections in Yugoslavia, Greece, Turkey …
[PDF][PDF] Extent, duration, and nature of the Permian-Triassic superanoxic event
PB Wignall, RJ Twitchett, C Koeberl… - … -Geological Society of …, 2002 - researchgate.net
The widespread development of anoxic and dysoxic deposition in marine settings occurred
during the Permian-Triassic (P-Tr) transition interval. Facies varied according to …
during the Permian-Triassic (P-Tr) transition interval. Facies varied according to …
The protracted Permo-Triassic crisis and multi-episode extinction around the Permian–Triassic boundary
H Yin, Q Feng, X Lai, A Baud, J Tong - Global and Planetary Change, 2007 - Elsevier
The Permo-Triassic crisis was a major turning point in geological history. Following the end-
Guadalupian extinction phase, the Palaeozoic biota underwent a steady decline through the …
Guadalupian extinction phase, the Palaeozoic biota underwent a steady decline through the …
An integrated biostratigraphy (conodonts and foraminifers) and chronostratigraphy (paleomagnetic reversals, magnetic susceptibility, elemental chemistry, carbon …
The chronostratigraphy of Guandao section has served as the foundation for numerous
studies of the end-Permian extinction and biotic recovery in south China. Guandao section is …
studies of the end-Permian extinction and biotic recovery in south China. Guandao section is …