Gypsum formation

Gypsum is an important constituent of cap rock, an anhydrite-gypsum rock formation. Though gypsum deposits can be found in several countries, its largest producers are, the United States, France, Italy, Canada, Australia, and Great Britain.

Gypsum formation. Wellington Formation (Kansas) Show map of Kansas. The Wellington Formation is an Early Permian geologic formation in Kansas and Oklahoma. [2] The formation's Hutchinson Salt Member is more recognized by the community than the formation itself, and the salt is still mined in central Kansas. [3]

13 Şub 2020 ... Those close to the mining and construction industries are familiar with gypsum as an important industrial mineral and product, ...

Gypsum is one of the most common and troublesome inorganic mineral scales in membrane systems, however, no mechanistic model is available to accurately predict the induction time of gypsum crystallization and inhibition. In this study, a new gypsum crystallization and inhibition model based on the classical nucleation theory and a Langmuir type ...Gypsum is considered both a sedimentary rock and a mineral. Its chemical formula is CaSO 4 ∙2H 2 O. Because gypsum formed when ancient seas evaporated in Oklahoma during Permian time (299-251 million years ago), geologists classify it as an evaporite. Western Oklahoma has many large deposits of gypsum totaling trillions of tons (Figure 1).Gypsum occurs in nature as flattened and often twinned crystals, and transparent, cleavable masses called selenite. Selenite contains no significant selenium; rather, both substances were named for the ancient Greek word for the Moon. Selenite may also occur in a silky, fibrous form, in which case it is commonly … See moreSchematic illustration of a scenario explaining the deposition of the Primary Lower Gypsum (PLG) evaporites. Gypsum precipitates within shallow-water levels and is preserved in shallow settings while the deep basins are characterized by dolomite formation and gypsum resedimenation. Modified from De Lange and Krijgsman (2010).Dark red sandstone and maroon siltstone, interbedded with shale, can be seen along the Belle Fourche River. Oxidation of iron-rich minerals causes the red color of the rocks. This rock layer is the Spearfish Formation. Above the Spearfish Formation is the Gypsum Springs Formation. As mineral rich water evaporated deposits of gypsum were left ...Does gypsum formation during sulfate attack on concrete lead to expansion? Cement and Concrete Research, 2000, 30: 117–123. Article Google Scholar Wilby, C.B., Concrete Materials and Structures. Cambridge University Press, 1991. Tsivilis, S., Sotiriadis, K. and Skaropoulou, A., Thaumasite form of sulfate attack (TSA) in limestone cement …Gypsum and anhydrite are primarily formed from hypersaline bodies of water. Gypsum is found in economic quantities and purities from the Upper Amaranth ...Gypsum occurs in two main varieties as white earthy masses or as clear crystals. In crystal form, its softness and single perfect cleavage with two less well-developed cleavage directions usually serve to distinguish gypsum from other similar-looking minerals. Anhydrite: When gypsum loses its water component, it forms the mineral anhydrite (CaSO4).

Elements that Form Gypsum. Gypsum is made up of oxygen, sulfur, calcium and water. As evaporation occurs the sulfur is not protected by the water and oxygen contacts sulfur bonding with it to form a sulfate (SO4 2). The sulfate then bonds with calcium (Ca) and water (H2O) to create gypsum.The precipitated calcium lactate requires acidification by strong acids, resulting in large amounts of acid consumption and gypsum formation. In recent decades, some modern methods such as electrodialysis, modified reactive distillation, anion exchange and membrane bioreactor have been reported in the literature (Datta and Henry, 2006).tify and quantify gypsum formation in marine sediments (Pir-let et al., 2010) as well as different sediment clast deposition in a glacio-lacustrine varved context (Bendle et al., 2015). High-elevation lakes situated in mountain areas are of-ten characterized by elevated and highly variable sedimen-Published by Copernicus Publications on behalf of the European …Elements that Form Gypsum. Gypsum is made up of oxygen, sulfur, calcium and water. As evaporation occurs the sulfur is not protected by the water and oxygen contacts sulfur bonding with it to form a sulfate (SO4 2). The sulfate then bonds with calcium (Ca) and water (H2O) to create gypsum.Gypsum is first crushed, heat-dried and then powdered. 1. Gypsum is used as fertilizer. 2. Gypsum prevents soil erosion, improves soil composition, helps the movement of water and air, and facilitates root growth. 3. Gypsum balances micronutrients like zinc, iron etc. 4.

Apr 16, 2020 · The gypsum scale formation studies, included three blank experiments (A,B,C) and a gypsum scale inhibition test run in presence of PAA-F1 (GSI), Table 2, Figure 3, Figure 4, Figure 5, Figure 6, Figure 7, Figure 8 and Figure 9. Each of the blank experiments had its own objective. Gypsum is calcium sulfate dihydrate (CaSO 4 2H 2 O). It is a natural mineral that occurs in certain types of sedimentary rocks. Gypsum forms when water evaporates in mineral-rich marine soil environments. Over long periods of time, evaporation brings more minerals to the soil surface, eventually forming a solid deposit.A previous study measured the δ 34 S values of authigenic gypsum and pyrite in sediments from gas hydrate-bearing site GMGS2–08 in the South China Sea (SCS; Fig. 1) and attributed the gypsum formation to pyrite oxidation and calcium exclusion during methane hydrate formation (Lin et al., 2016b). Nevertheless, additional studies are required ...This paper addresses one central issue of building stone research: an origin for calcium in gypsum formation in noncalcareous sandstones.ABSTRACT. Protecting the integrity of the wellbore is a major challenge for the sustainable development of hydrocarbon resources in nitrate formation. In this paper, A numerical model for investigating the effects of casing eccentricity on inclined wellbore integrity in salt-gypsum formation is developed. The effects of creep time, eccentricity distance, cement sheath modulus of elasticity and ...This paper investigates the influence of pH on the formation of gypsum. The system of CaO-SO3-Na2O-H2O was designed to analyse the precipitation of calcium ions with sulfate ions as gypsum in ...

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Elements that Form Gypsum. Gypsum is made up of oxygen, sulfur, calcium and water. As evaporation occurs the sulfur is not protected by the water and oxygen contacts sulfur bonding with it to form a sulfate (SO4 2). The sulfate then bonds with calcium (Ca) and water (H2O) to create gypsum.The effects of temperature on the formation of gypsum crystals were also investi-gated. Figure 4 shows the effect of temperature on the re action rate, the higher the tem-The determining factors of the formation of a precipitate can vary. Some reactions depend on temperature, such as solutions used for buffers, whereas others are dependent only on solution concentration. ... What is the equilibrium state of this solution with respect to gypsum? Solution. The ion product \[Q_s = (8.4 \times 10^{–5})(7.2 \times ...Gypsum is a non-metallic mineral, found in rock form. It is composed of 79.1% calcium sulphate and 20.9% water, by weight. Chemists call it Hydrous Calcium Sulphate, and as there is one molecule of calcium sulphate combined with two molecules of water. It has the chemical formula CaSO 4 2H 2 0. By volume this works out to nearly 50% water in ...Nov 7, 2016 · The group reported that gypsum actually forms in a three-step process: precipitation of nanocrystals of bassanite — or calcium sulfate hemihydrate, with one water molecule for every two calcium sulfate units — followed by the assembly of those crystals into larger aggregates, and finally transformation of the aggregates into gypsum. composes 42 percent of the formation, gypsum 40 percent, limestone. 17 percent ... gypsum bed near the middle of the formation, the gypsum is in thin to thick ...

Dec 2, 2006 · The deterioration of buildings and monuments by gypsum is the result of crystallization cycles of this salt. Although gypsum can dehydrate to a hemihydrate, the mineral bassanite, and to an anhydrate, the mineral anhydrite, this reaction occurs in nature on a geological time scale and therefore it is unlikely to occur when gypsum is found on and in building materials. The CaSO4–H2O system ... Gypsum Crystal Formation Underground. Cancel. Gypsum Crystal Formation · ABOUT · GA PUBLICATIONS AT-A-GLANCE · AIA CONTINUING EDUCATION · ICC CONTINUING ...Note also the disruption of the laminae as a result of desiccation and gypsum formation. (d) Photomicrograph of a part of sample (c) under normal light showing calcite pseudomorphs after lenticular gypsum, microbial laminae and microcrystalline dolomite. Circular objects in the dark microbial laminae are calcispheres believed to be green algal ...You might have music files on a music CD that you would also like to have on an mp3 player. Or, you might have a collection of older CDs that you would like to convert into a more modern format. Either way, this process is easy.Gypsum is a soft sulfate mineral composed of calcium sulfate dihydrate, with the chemical formula CaSO 4 ·2H 2 O. It is widely mined and is used as a fertilizer and as the main constituent in many forms of plaster , drywall and blackboard or sidewalk chalk .Creep deformation of the composite salt-gypsum formation occurs over time. Moreover, it applies excess stress on the wellbore casing, which can lead to casing damage. In this study, triaxial experiments are conducted on samples of salt-gypsum composite rock, and a power-law creep constitutive model is created.uniformgroundstresshavenotbeensolvedanalytically.One mightarguethatnon-uniformstressesdonotactdirectlyon thecasing,sotheproblemdoesnotexist,anditdoesnotThe formation of gypsum, from concentrated aqueous solutions of calcium sulfate, was thought to be a simple, single-step process. However, a group of European geochemists has now shown that gypsum ...A previous study measured the δ 34 S values of authigenic gypsum and pyrite in sediments from gas hydrate-bearing site GMGS2–08 in the South China Sea (SCS; Fig. 1) and attributed the gypsum formation to pyrite oxidation and calcium exclusion during methane hydrate formation (Lin et al., 2016b). Nevertheless, additional studies are required ...Most gypsiferous soils are located in arid areas, some in semi-arid ones. The presence of gypsum reflects the characteristic of wetness that was present in geological time, or it is actually related to the presence of a brackish water-table. River beds and lagoons are ideal locations for the formation of secondary gypsum deposits.

The formation of gypsum, from concentrated aqueous solutions of calcium sulfate, was thought to be a simple, single-step process. However, a group of European geochemists has now shown that gypsum ...

Gypsum is a fertilizer product and supplies the crop-available form of calcium (Ca 2 +) and sulfur (SO 4 2-). If these forms are deficient in soil, then crop productivity will benefit if gypsum is applied. This is a big "if" for Iowa soils. Research has not shown deficiency of Ca and normally any potential problem with low Ca levels is taken ...This paper investigates the influence of pH on the formation of gypsum. The system of CaO-SO3-Na2O-H2O was designed to analyse the precipitation of calcium ions with sulfate ions as gypsum in ...Nov 7, 2016 · The group reported that gypsum actually forms in a three-step process: precipitation of nanocrystals of bassanite — or calcium sulfate hemihydrate, with one water molecule for every two calcium sulfate units — followed by the assembly of those crystals into larger aggregates, and finally transformation of the aggregates into gypsum. The determining factors of the formation of a precipitate can vary. Some reactions depend on temperature, such as solutions used for buffers, whereas others are dependent only on solution concentration. ... What is the equilibrium state of this solution with respect to gypsum? Solution. The ion product \[Q_s = (8.4 \times 10^{–5})(7.2 \times ...The formation and dissolution of salt giants impacts ocean chemistry on thousand-million year timescales. Gypsum precipitation and weathering changes the oceanic calcium concentration with ...Gypsum is an evaporite mineral most commonly found in layered sedimentary deposits in association with halite, anhydrite, sulfur, calcite, and dolomite. Gypsum (CaSO 4. 2H 2 O) is very similar to Anhydrite (CaSO 4). The chemical difference is that gypsum contains two waters and anhydrite is without water. Gypsum is the most common sulfate mineral. Rouleaux formation happens when either fibrinogens or globulins are present at high levels in the blood, although at times it may be caused by incorrect blood smear preparation when blood is placed on a slide for microscopic examination.MLA formatting refers to the writing style guide produced by the Modern Language Association. If you’re taking a class in the liberal arts, you usually have to follow this format when writing papers. In addition to looking at MLA examples, ...Dec 30, 2019 · Although gypsum is usually considered a typical evaporitic mineral, non-evaporitic gypsum formation can also take place in (deep) marine sediments due to a variety of mechanisms such as, mixing of seawaters coupled to the dissolution of foraminiferal ooze (Briskin and Schreiber, 1978), salt diapirism (Haffert et al., 2013; Haffert and Haeckel, 2019), oxidation of sedimentary sulfide minerals ...

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The deterioration of buildings and monuments by gypsum is the result of crystallization cycles of this salt. Although gypsum can dehydrate to a hemihydrate, the mineral bassanite, and to an anhydrate, the mineral anhydrite, this reaction occurs in nature on a geological time scale and therefore it is unlikely to occur when gypsum is found on and in building materials. The CaSO4–H2O system ...This work firstly shows that the observed crystallization inside of gypsum during dehydration is the formation of alpha-hemihydrate. Keywords: -hemihydrate; -hemihydrate; calcium sulfate dihydrate; crystallization inside crystal; fiber gypsum formation 1. Introduction Gypsum is one of the most used inorganic binding materials in the world. It ...Jan 30, 2021 · Gypsum (CaSO4·2H2O) is the most common sulfate mineral on Earth and is also found on Mars. It is an evaporitic mineral that predominantly precipitates from brines. In addition to its precipitation in natural environments, gypsum also forms an undesired scale in many industrial processes that utilize or produce brines. Thus, better insights into gypsum formation can contribute to the ... The salt formation is a set of gray and ochre mudstone, siltstone, mud gypsum, hard gypsum, calcium mannite, and other salt rocks, buried at a depth of 200–400 m. The thickness of the salt section controlled by drilling is 348.72–554.76 m.The formation consists of up to 300 feet (91 m) of gypsum or anhydrite with a few thin beds of limestone. The formation is found within the Delaware Basin and was deposited after the formation of the Capitan Formation, the fossil reef defining the margins of the Delaware Basin.ABSTRACT. Protecting the integrity of the wellbore is a major challenge for the sustainable development of hydrocarbon resources in nitrate formation. In this paper, A numerical model for investigating the effects of casing eccentricity on inclined wellbore integrity in salt-gypsum formation is developed. The effects of creep time, eccentricity distance, cement sheath modulus of elasticity and ...The precipitated calcium lactate requires acidification by strong acids, resulting in large amounts of acid consumption and gypsum formation. In recent decades, some modern methods such as electrodialysis, modified reactive distillation, anion exchange and membrane bioreactor have been reported in the literature (Datta and Henry, 2006).This work firstly shows that the observed crystallization inside of gypsum during dehydration is the formation of alpha-hemihydrate. Keywords: -hemihydrate; -hemihydrate; calcium sulfate dihydrate; crystallization inside crystal; fiber gypsum formation 1. Introduction Gypsum is one of the most used inorganic binding materials in the world. It ...The precipitated calcium lactate requires acidification by strong acids, resulting in large amounts of acid consumption and gypsum formation. In recent decades, some modern methods such as electrodialysis, modified reactive distillation, anion exchange and membrane bioreactor have been reported in the literature (Datta and Henry, 2006).... applied axial load. a on deformation during the formation of gypsum. While hydration of bassanite involves a solid volume increase, gypsum exhibits ... ….

Gypsum is calcium sulfate dihydrate (CaSO 4 2H 2 O). It is a natural mineral that occurs in certain types of sedimentary rocks. Gypsum forms when water evaporates in mineral-rich marine soil environments. Over long periods of time, evaporation brings more minerals to the soil surface, eventually forming a solid deposit. The Castile formation consists largely of anhydrite, which is marked throughout by thin, light and dark laminae that may be varves. 16 These laminae are best seen in well cores, but appear also in all reasonably fresh exposures of the formation, even where the rock has altered to gypsum. The light-colored laminae are relatively pure anhydrite ...The formation of gypsum (CaSO 4 •2H 2 O) from solution is generally assumed to proceed via a single-step direct precipitation pathway , although a multistep pathway including an amorphous intermediate has been reported. One current limitation in quantifying and controlling this reaction is the lack of a mechanistic understanding of the stages ...3 Eyl 2020 ... To investigate the precipitation kinetics of the formation of Ca2SO4·2H2O (gypsum) the following reaction was carried out: Solutions of 50 ...Gypsum (CaSO 4 ·2H 2 O) is an ideal material to study these processes. It forms rapidly at room temperature via bassanite (CaSO 4 · [1/2]H 2 O) hydration and is commonly used as an analog for rocks in high-temperature, high-pressure conditions.1. Introduction. Textural observations, and compositional analyses of veins are important for understanding the vein formation processes. Veins filled with gypsum often consist of a median zone with fiber zones on both sides of it (Fig. 2 f), which is a distinctive feature of antitaxial fibrous veins (Bons et al., 2012).The formation pathways of gypsum remain uncertain. Here, using truly in situ and fast time-resolved small-angle X-ray scattering, we quantify the four-stage solution-based nucleation and growth of ...Gypsum (CaSO4·2H2O) is the most common sulfate mineral on Earth and is also found on Mars. It is an evaporitic mineral that predominantly precipitates from brines. In addition to its precipitation in natural environments, gypsum also forms an undesired scale in many industrial processes that utilize or produce brines. Thus, better insights into gypsum formation can contribute to the ...gypsum occur simultaneously. K Serafeimidis established a strict anhydrite-gypsum-water thermodynamic equilibrium equation, proving that gypsum formation caused by water absorption of clay minerals is the main process of sulfate-bearing mineral mudstone expansion. Mudstone contains the structural characteristics of both soil and … Gypsum formation, Gypsum (CaSO4·2H2O) is the most common sulfate mineral on Earth and is also found on Mars. It is an evaporitic mineral that predominantly precipitates from brines. In addition to its precipitation in natural environments, gypsum also forms an undesired scale in many industrial processes that utilize or produce brines. Thus, better insights into gypsum formation can contribute to the ... , The formation consists of up to 300 feet (91 m) of gypsum or anhydrite with a few thin beds of limestone. The formation is found within the Delaware Basin and was deposited after the formation of the Capitan Formation, the fossil reef defining the margins of the Delaware Basin., Dolomite has a Mohs hardness of 3 1/2 to 4 and a specific gravity of 2.85 ± 0.01. Some dolomites are triboluminescent. The dolomite of most dolostones is granular, with the individual grains ranging in size from microscopic up to a few millimetres across. Most dolomite marbles are coarsely granular with individual grains ranging between 2 and ..., Most gypsiferous soils are located in arid areas, some in semi-arid ones. The presence of gypsum reflects the characteristic of wetness that was present in geological time, or it is actually related to the presence of a brackish water-table. River beds and lagoons are ideal locations for the formation of secondary gypsum deposits. , The formation of gypsum in commercial quantities can generally be ascribed to one of three causes: Transformation of deposits, generally limestone, by chemical reactions involving weak solutions of sulfuric acid; precipitation from sea water, due primarily to concentration by evaporation; or reactions between the salts in solution., DensGlass sheathing is a gold-colored fiberglass mat gypsum panel that raises the performance and adds long-lasting qualities to fire-rated and nonfire-rated building fabrications. The sheathings provide protection against moisture and mold..., Mar 11, 2020 · Gypsum roses tend to have sharper edges better defined than baryt roses. Celestine and other minerals bladed with evaporite may also form clusters of rosettes. These can either appear as a single rose-like bloom, or as bloom clusters, with most sizes ranging from pea size to 4 inches (10 cm) in diameter. , The formation of calcium sulfate minerals (gypsum, anhydrite, and bassanite) is a common process in both natural and engineered settings. It plays a key role in the global sulfur cycle in the environment, and has been employed since antiquity in construction and architecture [ 3 ]., Gypsum (calcium sulfate dihydrate) is one of the most used inorganic binding materials in the world. During calcination, calcium sulfate subhydrates are formed and, for technical reasons, are mixed with water to form dihydrate again. Therefore, the dehydration process of gypsum and the rehydration of hemihydrate were investigated. This dehydration process is technically performed in three ..., The Sawa Lake, a biodiverse wetland situated near the city of Samawa, south of the capital Baghdad. The lake has been formed over limestone rock and studded with gypsum formations. It has no inlet or outlet and the source of its waters had mystified experts for centuries, fuelling fantastical folklore and religious tales that locals recite as ..., Sulfate attack on concrete is defined as the expansive reaction between penetrating sulfates and hardened binder phases. Expansion is generally attributed to the formation of ettringite and, at high sulfate concentrations, gypsum [1], [2]. Ettringite forms when penetrating sulfates react with AFm. However, recent investigations on the ..., Sand Dune Formation - Sand dune formation occurs when wind blows sand against an obstacle. Learn how sand dune formation works and how a sand dune travels. Advertisement A sand dune needs the following three things to form: Where these thre..., , The formation pathways of gypsum remain uncertain. Here, using truly in situ and fast time-resolved small-angle X-ray scattering, we quantify the four-stage solution-based nucleation and growth of ..., Gypsum (CaSO 4 ·2H 2 O) is an ideal material to study these processes. It forms rapidly at room temperature via bassanite (CaSO 4 · [1/2]H 2 O) hydration and is commonly used as an analog for rocks in high-temperature, high-pressure conditions., Home / Trimless & Gypsum. Trimless & Gypsum. TZ 200 Light Fixture. TZ 200 · TZ T Round ceiling light. TZ T Round · TZ T Square ... Copyright © 2022 Formation ..., Gypsum (CaSO 4 ·2H 2 O) is an ideal material to study these processes. It forms rapidly at room temperature via bassanite (CaSO 4 · [1/2]H 2 O) hydration and is commonly used as an analog for rocks in high-temperature, high-pressure conditions., Although gypsum is usually considered a typical evaporitic mineral, non-evaporitic gypsum formation can also take place in (deep) marine sediments due to a variety of mechanisms such as, mixing of seawaters coupled to the dissolution of foraminiferal ooze (Briskin and Schreiber, 1978), salt diapirism (Haffert et al., 2013; Haffert and Haeckel, 2019), oxidation of sedimentary sulfide minerals ..., The Sr isotope data from the gypsum formation as a tectonic slice display the Late Triassic age of the Mediterranean belt (Gündoğan et al. 2008). The Neogene fill overlying unconformably the bedrock units is formed from ... (Turkey) and some recent sinkhole formation in its close vicinity (Kaklık Cave), 1st Int. WS on Role of …, While the mechanism for gypsum formation during falling water levels was established e.g. 13,15, the corresponding time interval in between the two major gypsum units, and its climatic ..., You might have music files on a music CD that you would also like to have on an mp3 player. Or, you might have a collection of older CDs that you would like to convert into a more modern format. Either way, this process is easy., gypsum formation until a large natural cavity was intercepted in an underground quarry near Moncalvo causing a catastrophic collapse at the surface. Here, these active phreatic conduits are ..., acid monomers and directly employed for gypsum scale inhibition. The formation of PPCA was verified by FTIR and 31PNMR spectroscopies, and then its inhibition performance was evaluated by the complexometric deter-mination of the Ca2þ concentration. The PPCA (2.5 ppm) showed 100% inhibition efficiency at a saturation index, Spread the loveMinerals are captivating treasures of the Earth, and among them, sulfate minerals shine with their unique properties and breathtaking beauty. As K …, @article{osti_1558621, title = {In Situ Transmission Electron Microscopy Explores a New Nanoscale Pathway for Direct Gypsum Formation in Aqueous Solution}, author = {He, Kun and Nie, Anmin and Yuan, Yifei and Ghodsi, Seyed Mohammadreza and Song, Boao and Firlar, Emre and Lu, Jun and Lu, Yu-peng and Shokuhfar, Tolou and Megaridis, Constantine M. and Shahbazian-Yassar, Reza}, abstractNote = {In ..., Gypsum. Gypsum, hydrated calcium sulphate, Ca SO4.2H2O, is a common mineral formed mainly by the evaporation of sea water. Known from antiquity, its name comes from the Arabic jips, for "plaster," then to the Greek gypsos, for chalk. Gypsum Crystal, unknown Locality. University of Waterloo Earth Sciences Museum Collection. , Gypsum is a fertilizer product and supplies the crop-available form of calcium (Ca 2 +) and sulfur (SO 4 2-). If these forms are deficient in soil, then crop productivity will benefit if gypsum is applied. This is a big "if" for Iowa soils. Research has not shown deficiency of Ca and normally any potential problem with low Ca levels is taken ..., Sep 12, 2023 · The type of formation created depends largely on whether the water is dripping, trickling, or seeping when it enters the cave passage. Gypsum speleothems form because water seeping into the cave often contains small amounts of gypsum (calcium sulfate, CaSO4) picked up from the limestone or overlying sandstone. , The goals of GYPWORLD are to (1) assess plant and lichen diversity associated with gypsum soils; (2) determine the origin of gypsophilic biotas worldwide; (3) understand …, The effects of temperature on the formation of gypsum crystals were also investi-gated. Figure 4 shows the effect of temperature on the re action rate, the higher the tem-, uniformgroundstresshavenotbeensolvedanalytically.One mightarguethatnon-uniformstressesdonotactdirectlyon thecasing,sotheproblemdoesnotexist,anditdoesnot, Although gypsum is usually considered a typical evaporitic mineral, non-evaporitic gypsum formation can also take place in (deep) marine sediments due to a variety of mechanisms such as, mixing of seawaters coupled to the dissolution of foraminiferal ooze (Briskin and Schreiber, 1978), salt diapirism (Haffert et al., 2013; Haffert and Haeckel, 2019), oxidation of sedimentary sulfide minerals ..., Gypsum Spring Formation, Nugget Sandstone, and Chugwater Formation (Lower Triassic-Upper Jurassic) at surface, covers < 0.1 % of this area. Gypsum Spring Formation - Interbedded red shale, dolomite, and gypsum. In north Wyoming wedges out south in T. 39 N. Nugget Sandstone (JTRn) - gray to dull-red, crossbedded quartz sandstone.