Results 141 to 150 of about 2,604 (197)

Bioavailable phosphite in the surface ocean during the Great Oxidation Event. [PDF]

open access: yesNat Commun
Baidya AS   +5 more
europepmc   +1 more source

The Lower Precambrian in the Structure of Paleozoids of the Subpolar Urals

Doklady Earth Sciences, 2019
Rocks of Early Precambrian age have been established in many polymetamorphic complexes of the Urals. However, there is no doubt that only two polymetamorphic complexes (Taratash and Aleksandrovsk), located on the western slope of the Urals, belong to the Archean–Paleoproterozoic sequence.
Yu. I. Pystina   +2 more
openaire   +1 more source

Geotectonic evolution of the Siberian platform during the Precambrian and comparison with the lower Precambrian complexes of eastern Asia

Journal of Southeast Asian Earth Sciences, 1990
Abstract The main stages of the geotectonic evolution during the Precambrian of the Siberian platform are older than those in the other blocks of eastern Asia. Upper Proterozoic orogenic stages took place in north China-Korean blocks near the collision boundary with the south China block. Such Upper Proterozoic stages are characteristic for the south
N.L. Dobretsov, V.L. Dook, V.I. Kitsul
openaire   +1 more source

Geology of lower Precambrian in Shilka-Olekma interstream area

International Geology Review, 1967
The area, an alternation of large synclinoria and anticlinoria, proves to be a direct southwest extension of the early Proterozoic Stanovoy folded zone, a differentiated geosynelinal downwarp with a radical structural unconformity to its deeply metamorphosed Archean base. — IGR Staff.
V.I. Shul'diner, A.F. Ozerskiy
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The discovery of retene in Precambrian and Lower Paleozoic marine formations

Chinese Journal of Geochemistry, 1995
Microscopic and SEM observations of thin sections and kerogens and GC-MS analyses of aromatic fractions in sediment extracts and pyrolysis products of kerogens provide strong evidence suggesting that in the Lower Yangtze Valley area the Sinian and Lower Paleozoic carbonate formations of marine facies received no higher plant input, but there was ...
Jiang Naihuang   +6 more
openaire   +1 more source

Upper Precambrian–Lower Cambrian biota from the northwest of Argentina

Geological Magazine, 1986
AbstractThe principal characters of the biota from Upper Precambrian–Lower Cambrian rocks in the northwest of Argentina are described. It is possible to observe two groups: the trace fossils and the medusoid impressions. At the same time, a regional palaeogeographical analysis is attempted as well as a comparison with outcrops of similar age from the ...
Florencio Gilberto Aceñolaza   +1 more
openaire   +1 more source

The Precambrian/Lower Cambrian pluton from Vila Nova

2010
The Vila Nova pluton is a small, Pre-Variscan granitic body that intruded rocks of the Central Iberian Zone near the contact with the Ossa Morena Zone and is affected by several shear zones and faults. Its contact metamorphic aureole is constituted by micaschist with porphyroblasts in the outer zone and hornfels in the inner zone.
Reis, A.I.M.   +2 more
openaire   +4 more sources

Problem of the lower Precambrian “greenstone belts”

International Geology Review, 1980
(1980). Problem of the lower Precambrian “greenstone belts”. International Geology Review: Vol. 22, No. 11, pp. 1314-1326.
openaire   +1 more source

Characteristics and evolution of the lower precambrian basement of the North China platform

Journal of Southeast Asian Earth Sciences, 1989
Abstract The Lower Precambrian basement of the North China platform is composed of Lower, Upper Archaean and Lower Proterozoic metamorphic complexes. The Lower Archaean metamorphic complex, distributed mainly in the North Border sub-domain, consists of granulite, gneiss, amphibolite and pyroxenite. The metamorphic grade is up to granulite facies. The
Cui Wenyuan   +3 more
openaire   +1 more source

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