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sediments
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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
bassanite
Jarosite formation in Permian-Triassic strata at Xiakou (South China): Implications for jarosite precipitation from H 2 S upwelling on Mars Available to Purchase
Elastic stresses can form metamorphic fabrics Available to Purchase
Chinleite-(Nd), NaNd(SO 4 ) 2 (H 2 O), the Nd Analogue of Chinleite-(Y) from the Markey Mine, Red Canyon, San Juan County, Utah, USA Available to Purchase
Mineral Composition of the Sediments of Lake Malye Chany as an Indicator of Holocene Climate Changes (Southern West Siberia) Available to Purchase
Phoxite, (NH 4 ) 2 Mg 2 (C 2 O 4 )(PO 3 OH) 2 (H 2 O) 4 , the first phosphate-oxalate mineral Available to Purchase
Gypsum, bassanite, and anhydrite at Gale crater, Mars Open Access
Chinleite-(Y), NaY(SO 4 ) 2 ·H 2 O, a new rare-earth sulfate mineral structurally related to bassanite Available to Purchase
A re-investigation of ardealite from the type locality, the “dry” Cioclovina Cave (Şureanu Mountains, Romania) Available to Purchase
THE RAMAN STUDY OF WEATHERING MINERALS FROM THE CORANDA-HONDOL OPEN PIT (CERTEJ GOLD-SILVER DEPOSIT) AND THEIR PHOTOCHEMICAL DEGRADATION PRODUCTS UNDER LASER IRRADIATION Available to Purchase
Carboxylic acids: effective inhibitors for calcium sulfate precipitation? Open Access
Spectral properties of Ca-sulfates: Gypsum, bassanite, and anhydrite Available to Purchase
Oskarssonite, AlF 3 , a new fumarolic mineral from Eldfell volcano, Heimaey, Iceland Available to Purchase
Experimental VNIR reflectance spectroscopy of gypsum dehydration: Investigating the gypsum to bassanite transition Available to Purchase
The Todilto Formation as an analog of short-lived Martian flood evaporites Available to Purchase
The Jurassic Todilto Formation of NW New Mexico and SW Colorado, USA, has utility as an analog of Martian flood evaporites. The Todilto Formation is a concentrically and vertically zoned carbonate (calcite with minor late dolomite) to sulfate (gypsum) evaporite deposit that developed over a short time span (10 4 –10 5 yr) after rapid flooding of the vast dune field of the Entrada Formation. Within the limits of the very different hydrogeologic environments of Mars and Earth, the Todilto setting of short-lived brine evolution in a largely eolian environment, with terminal formation of a salt hydrate common to both planets (gypsum), provides a useful field area for descriptive and petrogenetic studies of evaporite evolution and interaction with a porous, sandy substrate. The Todilto Formation has an added feature of interest in its association with bituminous materials that have likely microbial precursors, providing a brine-microorganism association that may represent a potential setting for primitive life as might be found on Mars.