The magnetic and color reflectance properties of hematite: From Earth to Mars
Hematite is a canted antiferromagnet with reddish color that occurs widely on Earth and
Mars. Identification and quantification of hematite is conveniently achieved through its …
Mars. Identification and quantification of hematite is conveniently achieved through its …
Cretaceous oceanic red beds (CORBs): Different time scales and models of origin
The Cretaceous oceanic red bed (CORB) is a newly opened window on global oceanic and
climate changes during the Cretaceous greenhouse world. As a result of the International …
climate changes during the Cretaceous greenhouse world. As a result of the International …
[HTML][HTML] 中国北方晚中生代陆相盆地红-黑岩系耦合产出对砂岩型铀矿成矿环境的制约
金若时， 程银行， 李建国， 司马献章， 苗培森， 王少轶… - 中国地质, 2017 - cgsjournals.com
为研究中国北方陆相盆地红层-黑色岩系对砂岩型铀成矿的制约, 文章研究了国内外红-
黑岩系与砂岩型铀矿赋存岩层的时空关系, 筛选了10 万余m 岩心钻探资料, 选择准噶尔 …
黑岩系与砂岩型铀矿赋存岩层的时空关系, 筛选了10 万余m 岩心钻探资料, 选择准噶尔 …
Upper Cretaceous oceanic red beds (CORBs) in the Tethys: occurrences, lithofacies, age, and environments
A major change in oceanic sedimentation from mid-Cretaceous organic carbon-enriched
deep-sea deposits to predominantly Upper Cretaceous oceanic red beds (CORBs) …
deep-sea deposits to predominantly Upper Cretaceous oceanic red beds (CORBs) …
Upper Cretaceous oceanic red beds in southern Tibet: a major change from anoxic to oxic, deep-sea environments
Red marine mudstones intercalated with pelagic marlstones, limestones and radiolarian
cherts comprise the Chuangde Formation, which overlies mid-Cretaceous dark grey shales …
cherts comprise the Chuangde Formation, which overlies mid-Cretaceous dark grey shales …
Cretaceous oceanic red beds as possible consequence of oceanic anoxic events
Oceanic Anoxic Events (OAEs) represent brief periods of burial of large amounts of organic
carbon in the oceans during Cretaceous time. Burial of organic carbon, which preferentially …
carbon in the oceans during Cretaceous time. Burial of organic carbon, which preferentially …
From black-and-white to colour in the Silurian
Ironstones and iron-rich limestones regularly occur as components of time-specific intervals
of the Palaeozoic as well as in younger times (Brett et al., 2012--this issue). Silurian …
of the Palaeozoic as well as in younger times (Brett et al., 2012--this issue). Silurian …
New paleomagnetic results from the Upper Cretaceous red marls of the Pieniny Klippen Belt, Western Carpathians: Evidence for general CCW rotation and …
The Pieniny Klippen Belt (PKB) is a narrow arcuate structure separating the Central and
Outer Western Carpathians formed during several Cenozoic deformational stages. The …
Outer Western Carpathians formed during several Cenozoic deformational stages. The …
The formation of marine red beds and iron cycling on the Mesoproterozoic North China Platform
Marine red beds (MRBs) are common in sedimentary records, but their genesis and
environmental implications remain controversial. Genetic models proposed for MRBs …
environmental implications remain controversial. Genetic models proposed for MRBs …
Iron bacterial and fungal mats, Bajocian stratotype (Mid-Jurassic, northern Normandy, France)
A Préat, B Mamet, C De Ridder, F Boulvain… - Sedimentary Geology, 2000 - Elsevier
The Oolithe ferrugineuse de Bayeux Formation is located at the historical Bajocian
stratotype of Sainte-Honorine-des-Pertes, north of Bayeux, Normandy. The condensed …
stratotype of Sainte-Honorine-des-Pertes, north of Bayeux, Normandy. The condensed …