作者: FOVEA 時(shí)間: 2025-3-21 22:31 作者: 小歌劇 時(shí)間: 2025-3-22 04:23
Book 2016Latest editions. Written by a field specialist in research and exploration, the book presents a comprehensive overview of the realms of low- and high-temperature evaporite evolution. It is aimed at earth science professionals, sedimentologists, oil and gas explorers, mining geologists as well as environmental geologists..作者: chastise 時(shí)間: 2025-3-22 07:39
Electrocardiography and Cardiac Drug Therapyydrological setting where salt beds tend to form is that typified by perennial subaqueous brine hydrologies (primary textures) in coastal and continental settings and this will be the focus of the next chapter.作者: Bereavement 時(shí)間: 2025-3-22 09:41 作者: GRIEF 時(shí)間: 2025-3-22 15:34
Andrew Krahn,Wael Alqarawi,Peter J. Schwartzteracts with and responds to the physical environment and has been in operation on the earth’s surface for at least the past 3.45 billion years. There is no need to invoke the supernatural and sky faeries to explain biological evolution and other earth processes, and there is no geological evidence 作者: GRIEF 時(shí)間: 2025-3-22 19:30
RF Bulk Acoustic Wave Resonators and Filtersrock volume (Duggan et al. 2001). Evaporites that enter the metamorphic realm can have an extensive influence consequent rock type and distribution, well after the primary sedimentary and diagenetic salts are long gone (.).作者: 浮雕 時(shí)間: 2025-3-23 00:17 作者: Tempor 時(shí)間: 2025-3-23 04:56
Rules and Modeling of Promotion,il and gas fields do not differ significantly. However, Grunau argues many “supergiant” gas accumulations below depths of 3,000 m and have either not yet been discovered, or have not yet been put in production (e.g. much of the Khuff-hosted gas in North Dome in the Middle East).作者: MAL 時(shí)間: 2025-3-23 09:34
https://doi.org/10.1007/978-3-642-34252-3thers have argued that ancient sylvite was sometimes a primary precipitate, deposited by the cooling of highly saline surface or near surface brines and from seawater with ionic proportions different to those of today (Hardie 1996).作者: 縱欲 時(shí)間: 2025-3-23 10:22 作者: Gullible 時(shí)間: 2025-3-23 14:27
Sabkhas, Saline Mudflats and Pans,ydrological setting where salt beds tend to form is that typified by perennial subaqueous brine hydrologies (primary textures) in coastal and continental settings and this will be the focus of the next chapter.作者: 停止償付 時(shí)間: 2025-3-23 18:28 作者: alliance 時(shí)間: 2025-3-23 23:22
Ancient Basins and Stratigraphic Evolution,teracts with and responds to the physical environment and has been in operation on the earth’s surface for at least the past 3.45 billion years. There is no need to invoke the supernatural and sky faeries to explain biological evolution and other earth processes, and there is no geological evidence 作者: progestogen 時(shí)間: 2025-3-24 06:24
Hypersaline Fluid Evolution During Burial and Uplift,rock volume (Duggan et al. 2001). Evaporites that enter the metamorphic realm can have an extensive influence consequent rock type and distribution, well after the primary sedimentary and diagenetic salts are long gone (.).作者: 萬(wàn)靈丹 時(shí)間: 2025-3-24 08:30 作者: 輕浮思想 時(shí)間: 2025-3-24 10:45 作者: hankering 時(shí)間: 2025-3-24 18:23 作者: photophobia 時(shí)間: 2025-3-24 19:33
Meta-evaporites, and siliciclastic clays. “After” metamorphism, typically driven by subduction and continent-continent collision, the end product of this once dominantly NaCl body of rock is a series of sodic and magnesian aluminosilicates, magnesites, calc-silicates and marbles with local zones of potassic enrichm作者: BROTH 時(shí)間: 2025-3-25 00:12 作者: Accolade 時(shí)間: 2025-3-25 03:28 作者: Judicious 時(shí)間: 2025-3-25 09:48 作者: SHOCK 時(shí)間: 2025-3-25 12:52
Electrocardiography and Cardiac Drug Therapyabkhas) and saline pans. These two settings encompass that part of the hydrological spectrum dominated by capillary and ephemeral at-surface brine hydrologies. Climatically, these settings tend to occur in arid deserts (K?ppen zone: BW) in both coastal and continental interior arid settings where sa作者: 惡名聲 時(shí)間: 2025-3-25 16:28
https://doi.org/10.1007/978-981-15-3699-1pan settings discussed in the previous chapter, when we seek equivalence in the Quaternary record we find our marine-fed choices are limited both in number and scale (Fig. 4.1; Table 4.1). If we consider all nonmarine and marine saline perennial water masses in modern systems as suitable for discuss作者: cultivated 時(shí)間: 2025-3-25 23:44
Andrew Krahn,Wael Alqarawi,Peter J. Schwartznteenth century, when Werner’s Neptunist postulates explained world geology (including igneous strata) as layered precipitates from cooling oceanic waters. And, like Werner’s Scottish antagonists, we are still discussing the merits of strict uniformitarianism. In this chapter I am not questioning th作者: Accord 時(shí)間: 2025-3-26 00:50
Ke Ke,Gang Wang,Dianxue Cao,Guoxiong Wang, Gulf of Mexico, North Sea, Lower Congo Basin, Santos Basin and Zagros). An understanding of the physics of salt and how salt flow influences tectonics and sedimentation is therefore critical to effective and efficient petroleum exploration (.). And, I would argue, is also critical to a significant作者: DOSE 時(shí)間: 2025-3-26 08:09 作者: CODE 時(shí)間: 2025-3-26 12:19 作者: harrow 時(shí)間: 2025-3-26 14:33 作者: harpsichord 時(shí)間: 2025-3-26 17:44
Rules and Modeling of Promotion,the other half are sealed by shales (Fig. 10.1; Grunau 1987). Kirkland and Evans (1981) argued that evaporites overlie or seal carbonates containing an estimated 50 % of the world’s known total petroleum reserve. Of the world’s 25 largest gas fields, nine are sealed by evaporites and sixteen by shal作者: Psa617 時(shí)間: 2025-3-26 23:44
https://doi.org/10.1007/978-3-642-34252-3rface (primary salts) or in the shallow subsurface (secondary salts). Today, bedded accumulations of primary potash evaporites are a relatively rare occurrence. Extremely high solubility of most potash salts means they accumulate in highly restricted, some would say highly continental, modern deposi作者: CODA 時(shí)間: 2025-3-27 02:01
Effective Transport Properties,y greenschist phase, little or nothing of the original sedimentary mineral phase remains with the possible exception of anhydrite (Table 14.1; Spear 1993). Consider “the before and after” situation as a sequence of evaporite-entraining sediments passes into the metamorphic realm. Under a likely “bef作者: convert 時(shí)間: 2025-3-27 07:18
Patrick G. Grimes,Richard J. Bellows,M. Zahnent and entrapment in subsurface settings ranging from the burial diagenetic through to the metamorphic and igneous realms. Within this framework, this chapter explores relationships between evaporites and lower temperature ore deposits, where ore is defined as a mineral, or an aggregate of minerals作者: 高談闊論 時(shí)間: 2025-3-27 12:01 作者: LUDE 時(shí)間: 2025-3-27 14:57 作者: 雕鏤 時(shí)間: 2025-3-27 20:25 作者: 反饋 時(shí)間: 2025-3-28 01:34 作者: 緩和 時(shí)間: 2025-3-28 03:27 作者: Hiatal-Hernia 時(shí)間: 2025-3-28 06:19 作者: 固執(zhí)點(diǎn)好 時(shí)間: 2025-3-28 11:10
Sabkhas, Saline Mudflats and Pans,abkhas) and saline pans. These two settings encompass that part of the hydrological spectrum dominated by capillary and ephemeral at-surface brine hydrologies. Climatically, these settings tend to occur in arid deserts (K?ppen zone: BW) in both coastal and continental interior arid settings where sa作者: recession 時(shí)間: 2025-3-28 16:30 作者: 十字架 時(shí)間: 2025-3-28 20:32
Ancient Basins and Stratigraphic Evolution,nteenth century, when Werner’s Neptunist postulates explained world geology (including igneous strata) as layered precipitates from cooling oceanic waters. And, like Werner’s Scottish antagonists, we are still discussing the merits of strict uniformitarianism. In this chapter I am not questioning th作者: 一致性 時(shí)間: 2025-3-29 01:10
Flowing Salt: Halokinesis,, Gulf of Mexico, North Sea, Lower Congo Basin, Santos Basin and Zagros). An understanding of the physics of salt and how salt flow influences tectonics and sedimentation is therefore critical to effective and efficient petroleum exploration (.). And, I would argue, is also critical to a significant作者: 哎呦 時(shí)間: 2025-3-29 05:43 作者: 盡責(zé) 時(shí)間: 2025-3-29 10:28
Hypersaline Fluid Evolution During Burial and Uplift,in subsequent hydrological stages in a sedimentary system containing thick salt, that is, rock-fluid interactions in an evaporite-entraining sequence experiencing ongoing burial, followed by possible uplift (mesogenesis followed by telogenesis. Thick, buried and dissolving evaporites influence subsu作者: 親愛(ài) 時(shí)間: 2025-3-29 13:45
Halotolerant Life in Feast or Famine: Organic Sources of Hydrocarbons and Fixers of Metals, form commercial accumulations of oil or gas (Fig. 9.1a). Back in 1981, Kirkland and Evans made the observation that some 50 % of the world’s oil sequestered in carbonate reservoirs may be associated with mesohaline micritic source rocks. Heresy or not, the notion that much of the oil in carbonate r作者: 不連貫 時(shí)間: 2025-3-29 18:32 作者: Optic-Disk 時(shí)間: 2025-3-29 20:06 作者: attenuate 時(shí)間: 2025-3-30 02:13 作者: Congeal 時(shí)間: 2025-3-30 07:36 作者: 漂亮 時(shí)間: 2025-3-30 11:02
Magma-Evaporite-Hydrothermal Metal Associations,ell documented, nor well understood. Mostly, this is because little or no actual salt remains once these high temperature interactions have run their course. On top of that, some hard-rock geologists with a career working in igneous and metamorphic terranes may not be well versed in sedimentary evap作者: 震驚 時(shí)間: 2025-3-30 12:51
geology.Contains numerous color figures.The monograph offers a comprehensive discussion of the role of evaporites in hydrocarbon generation and trapping, and new information on low temperature and high temperature ores. It also provides a wealth of information on exploitable salts, in a comprehensiv作者: 讓步 時(shí)間: 2025-3-30 18:09 作者: Explicate 時(shí)間: 2025-3-30 22:31
Magma-Evaporite-Hydrothermal Metal Associations,course. On top of that, some hard-rock geologists with a career working in igneous and metamorphic terranes may not be well versed in sedimentary evaporites or their meta-evaporitic siblings. The term pyrometasomatic encompasses some, but not all, of the types of salt-magma interaction that are the focus of this chapter.作者: CHYME 時(shí)間: 2025-3-31 01:44 作者: 保守黨 時(shí)間: 2025-3-31 06:10
Ke Ke,Gang Wang,Dianxue Cao,Guoxiong Wang portion of the world’s base and precious metal occurrences (see Chaps. . and .). Halokinetic salt is also a resource in salt, potash, gypsum and nitrate extraction (Chaps. . and .). Salt dome salt has the potential to be employed as a repository for radioactive and other wastes, and can act as a highly efficient seal to sequestered CO. (.).作者: 苦澀 時(shí)間: 2025-3-31 11:26
