Results 141 to 150 of about 5,331 (209)

Paleozoic carbonatites controlled rare-earth-elements mineralization at Bayan Obo. [PDF]

Sci Adv
Li Y, Wu LG, Yu Y, Yang L, Selby D, Li XH.   +5 more
europepmc   +1 more source

Process and forces of tight-sandstone gas charging in the Shihezi formation (P₂x¹) Dongsheng gas field, northern Ordos Basin China. [PDF]

Sci Rep
Cao Q, He F, Zhang W, Ye J, Lu Y, Liu Y, Yu H, An C, Sun L.   +8 more
europepmc   +1 more source

Buried, not erased: palynofloras in ultra-high-pressure metamorphic rocks. [PDF]

Sci Rep
Carosi R, Montomoli C, Iaccarino S, Dana D, Corno A, De Cesari F, Spina A.   +6 more
europepmc   +1 more source

A foundation model for rock thin-section images analysis. [PDF]

Commun Eng
Fan J, Yu X, Di Y, Lv T, Zhang R, Bao J, Liu Y, Li L, Pan X.   +8 more
europepmc   +1 more source

Repeated occurrences of marine anoxia under high atmospheric O₂ and icehouse conditions. [PDF]

Proc Natl Acad Sci U S A
Chen J, Li S, Zhang S, Isson T, Dahl TW, Planavsky NJ, Zhang F, Wang XD, Shen SZ, Montañez IP.   +9 more
europepmc   +1 more source

Tracking gas migration using reservoir PVT data as reality check for migration models. [PDF]

Sci Rep
Arouri KR, Schmidt R, Elouair Y, Nasser K, Tafsiri H, Alqahtani SA.   +5 more
europepmc   +1 more source

Paleoenvironmental reconstruction of the Middle Ordovician Majiagou Formation in the northeastern Ordos Basin and its effect on organic matter enrichment. [PDF]

Sci Rep
Wang Y, Wang X, Liu W, Zhang T, Zhang D.
europepmc   +1 more source

New exceptionally preserved arthropod from the Furongian of Canada. [PDF]

BMC Biol
Bicknell RDC, Kimmig J, Goodman A, Turner T, Smith PM.   +4 more
europepmc   +1 more source

Enhanced marine biological pump as a trigger for the onset of the late Paleozoic ice age. [PDF]

Sci Adv
Zhang F, Pohl A, Elrick M, Wei GY, Cheng K, Crockford P, Fakhraee M, Lin YB, Li N, Wang XD, Shen SZ.   +10 more
europepmc   +1 more source

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Paleozoic foraminifera

BioSystems, 1991
The approximately 300 million years that make up Paleozoic time saw the evolution of eight of the fifteen recognized suborders of Foraminifera. Of the suborders present in the Paleozoic, seven are morphologically relatively simple, slowly evolving, and continued into Mesozoic and Cenozoic times to become the ancestoral lineages from which evolved ...
C A, Ross, J R, Ross
exaly   +3 more sources