The Triassic–Jurassic transition–A review of environmental change at the dawn of modern life
Abstract The Triassic–Jurassic transition, which is here broadly defined as extending from
the Late Triassic through the Early Jurassic (~ 237 Ma to 174 Ma), was an important interval …
the Late Triassic through the Early Jurassic (~ 237 Ma to 174 Ma), was an important interval …
Composition, environment, and economic value of the Permian to Cretaceous coated grains from Zagros and the Persian Gulf
M Naderi-Khujin, V Tavakoli - International Journal of Sediment Research, 2023 - Elsevier
Ooid grainstone/packstone carbonate facies of the Dalan, Kangan, and Arab formations are
the main hydrocarbon reservoirs in the Persian Gulf. Based on detailed petrographic and …
the main hydrocarbon reservoirs in the Persian Gulf. Based on detailed petrographic and …
[HTML][HTML] Mid-Norian to Hettangian record and time-specific oolites during the end-Triassic Mass Extinction at Wadi Milaha, Musandam Peninsula, United Arab …
I Urban, I Demangel, L Krystyn, M Calner… - Journal of Asian Earth …, 2023 - Elsevier
Abstract The end-Triassic Mass Extinction (ETME) is generally regarded as a consequence
of the environmental changes associated with the emplacement of the Central Atlantic …
of the environmental changes associated with the emplacement of the Central Atlantic …
Geochemistry of the Triassic–Jurassic lateritic bauxites of the Salt Range: implications for eastward extension of the Tethyan bauxite deposits into Pakistan
S Iqbal, M Bibi, M Wagreich - International Journal of Earth Sciences, 2023 - Springer
Bauxite deposits are residuals of intense lateritic weathering under warm and humid
palaeoclimates. The Triassic–Jurassic Boundary (TJB) interval in the Salt Range, Pakistan …
palaeoclimates. The Triassic–Jurassic Boundary (TJB) interval in the Salt Range, Pakistan …
End-Triassic storm deposits in the lacustrine Sichuan Basin and their driving mechanisms
J Zeng, T Zhang, ME Popa, Y Wang, X Zhang… - Science China Earth …, 2024 - Springer
Storm deposits or tempestites are event sequences formed by storms, requiring at least a
water temperature of 26.5° C. While inland lakes are unlikely to form storm deposits because …
water temperature of 26.5° C. While inland lakes are unlikely to form storm deposits because …
Multi-proxy provenance analyses of the Kingriali and Datta formations (Triassic–Jurassic Transition): Evidence for westward extension of the neo-tethys passive …
The Salt Range, in Pakistan, preserves an insightful sedimentary record of passive margin
dynamics along the NW margin of the Indian Plate during the Mesozoic. This study develops …
dynamics along the NW margin of the Indian Plate during the Mesozoic. This study develops …
The Steptoean Positive Carbon Isotope Excursion (SPICE), inorganic aragonite precipitation and sea water chemistry: Insights from the Middle–Late Cambrian Port au …
Abstract The Late Cambrian Steptoean Positive Carbon Isotope Excursion marks a time of
significant change in ocean chemistry and trilobite faunas. On the lead up to the carbon …
significant change in ocean chemistry and trilobite faunas. On the lead up to the carbon …
Facies character and evolution of a mixed carbonate–siliciclastic shelf: Upper Triassic–Lower Jurassic succession in the eastern Northern Calcareous Alps …
Western Tethys sedimentary successions constitute fundamental archives of Late Triassic–
Early Jurassic environmental, carbonate production and tectonic changes. During the Late …
Early Jurassic environmental, carbonate production and tectonic changes. During the Late …
[HTML][HTML] Decoupled δ13Ccarb and δ13Corg records at Triassic–Jurassic boundary interval in eastern Tethys: Environmental implications for spatially different global …
Y Ge - Geoscience Frontiers, 2021 - Elsevier
Although δ 13 C data (either δ 13 C carb or δ 13 C org) of many Triassic–Jurassic (TJ)
sections have been acquired, paired δ 13 C carb and δ 13 C org from continuous TJ …
sections have been acquired, paired δ 13 C carb and δ 13 C org from continuous TJ …
[PDF][PDF] Marine oolites as proxies for palaeoenvironmental reconstructions during extinction events.
I Urban - 2023 - portal.research.lu.se
Marine oolites as proxies for palaeoenvironmental reconstructions during extinction events.
Urban, Ingrid Page 1 Marine oolites as proxies for palaeoenvironmental reconstructions during …
Urban, Ingrid Page 1 Marine oolites as proxies for palaeoenvironmental reconstructions during …