Simulation Study on the Mining Conditions of Dissolution of Low
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Brine Evolution in Qaidam Basin, Northern Tibetan Plateau, and the Formation of Playas As Mars Analogue Site
45th Lunar and Planetary Science Conference (2014) 1228.pdf BRINE EVOLUTION IN QAIDAM BASIN, NORTHERN TIBETAN PLATEAU, AND THE FORMATION OF PLAYAS AS MARS ANALOGUE SITE. W. G. Kong1 M. P. Zheng1 and F. J. Kong1, 1 MLR Key Laboratory of Saline Lake Resources and Environments, Institute of Mineral Resources, CAGS, Beijing 100037, China. ([email protected]) Introduction: Terrestrial analogue studies have part of the basin (Kunteyi depression). The Pliocene is served much critical information for understanding the first major salt forming period for Qaidam Basin, Mars [1]. Playa sediments in Qaidam Basin have a and the salt bearing sediments formed at the southwest complete set of salt minerals, i.e. carbonates, sulfates, part are dominated by sulfates, and those formed at the and chlorides,which have been identified on Mars northwest part of basin are partially sulfates dominate [e.g. 2-4]. The geographical conditions and high eleva- and partially chlorides dominate. After Pliocene, the tion of these playas induces Mars-like environmental deposition center started to move towards southeast conditions, such as low precipitation, low relative hu- until reaching the east part of the basin at Pleistocene, midity, low temperature, large seasonal and diurnal T reaching the second major salt forming stage, and the variation, high UV radiation, etc. [5,6]. Thus the salt bearing sediments formed at this stage are mainly playas in the Qaidam Basin servers a good terrestrial chlorides dominate. The distinct change in salt mineral reference for studying the depositional and secondary assemblages among deposition centers indicates the processes of martian salts. migration and geochemical differentiation of brines From 2008, a set of analogue studies have been inside the basin. -
A 94–10Ka Pollen Record of Vegetation Change in Qaidam Basin
Palaeogeography, Palaeoclimatology, Palaeoecology 431 (2015) 43–52 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo A94–10 ka pollen record of vegetation change in Qaidam Basin, northeastern Tibetan Plateau Haicheng Wei a,QishunFana, Yan Zhao b,HaizhouMaa, Fashou Shan a,FuyuanAna,QinYuana a Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining 810008, China b Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China article info abstract Article history: Drill core (ISL1A) was obtained from the Qarhan Salt Lake in central eastern Qaidam Basin, northeastern Tibetan Received 19 May 2014 Plateau (NE TP). Fossil pollen and the lithology of the core sediment were analyzed in conjunction with AMS 14C Received in revised form 27 March 2015 and 230Th dating. The results indicated that Artemisia and Chenopodiaceae dominated the steppe/desert steppe Accepted 24 April 2015 vegetation developed around the lake between 94 and 51.2 ka, corresponding with the organic-rich silty clay de- Available online 4 May 2015 posited in the core sediments. Pediastrum continuously appeared in the core sediments between 94 and 51.2 ka, Keywords: indicating freshwater to oligohaline conditions of the paleo-Qarhan Lake during the late marine isotope stage Pollen record (MIS) 5, MIS 4, and early MIS 3. During the 51.2 to 32.5 ka period, Ephedra dominated shrub-desert vegetation Climate change expanded in the basin, while, Pediastrum disappeared in the core sediments. The core sediments consisted of in- Qaidam Basin terbedded layers of halite silt and clay-rich halite between 51.2 and 32.5 ka, signifying a shift toward drier hydro- Late Pleistocene logic conditions. -
1469 Vol 43#5 Art 03.Indd
1469 The Canadian Mineralogist Vol. 43, pp. 1469-1487 (2005) BORATE MINERALS OF THE PENOBSQUIS AND MILLSTREAM DEPOSITS, SOUTHERN NEW BRUNSWICK, CANADA JOEL D. GRICE§, ROBERT A. GAULT AND JERRY VAN VELTHUIZEN† Research Division, Canadian Museum of Nature, P.O. Box 3443, Station D, Ottawa, Ontario K1P 6P4, Canada ABSTRACT The borate minerals found in two potash deposits, at Penobsquis and Millstream, Kings County, New Brunswick, are described in detail. These deposits are located in the Moncton Subbasin, which forms the eastern portion of the extensive Maritimes Basin. These marine evaporites consist of an early carbonate unit, followed by a sulfate, and fi nally, a salt unit. The borate assemblages occur in specifi c beds of halite and sylvite that were the last units to form in the evaporite sequence. Species identifi ed from drill-core sections include: boracite, brianroulstonite, chambersite, colemanite, congolite, danburite, hilgardite, howlite, hydroboracite, kurgantaite, penobsquisite, pringleite, ruitenbergite, strontioginorite, szaibélyite, trembathite, veatchite, volkovskite and walkerite. In addition, 41 non-borate species have been identifi ed, including magnesite, monohydrocalcite, sellaite, kieserite and fl uorite. The borate assemblages in the two deposits differ, and in each deposit, they vary stratigraphically. At Millstream, boracite is the most common borate in the sylvite + carnallite beds, with hilgardite in the lower halite strata. At Penobsquis, there is an upper unit of hilgardite + volkovskite + trembathite in halite and a lower unit of hydroboracite + volkov- skite + trembathite–congolite in halite–sylvite. At both deposits, values of the ratio of B isotopes [␦11B] range from 21.5 to 37.8‰ [21 analyses] and are consistent with a seawater source, without any need for a more exotic interpretation. -
Present Response of Qarhan Salt Flat to the Watershed Hydroclimate: the Key to Understanding Past Conditions for Evaporitic Deposit Formation
Abstract by JunQing Yu oral presentation_15th East Eurasia International Workshop, Busan, Korea 2018 PRESENT RESPONSE OF QARHAN SALT FLAT TO THE WATERSHED HYDROCLIMATE: THE KEY TO UNDERSTANDING PAST CONDITIONS FOR EVAPORITIC DEPOSIT FORMATION JunQing Yu1,2*, Lisha Zhang1,2, Chunliang Gao1,2, Rongchang Hong1,3, Aiying Cheng1,2 1 Key Laboratory of Comprehensive and Highly Efficient Utilization of Salt Lake Resources, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining 810008, China 2 Qinghai Provincial Key Laboratory of Geology and Environment of Salt Lakes, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining 810008, China 3 University of Chinese Academy of Sciences, Beijing 100049, China Correspondence: [email protected]; Tel.: +86-971-630-7153 Qarhan Salt Flat is the largest potash deposit in China and covers an area of 5856 km2 of the Qaidam Basin in the nothern Tibet-Qinghai Plateau. Although efforts on the study of the evaporite deposit were tremendous in the past 60 years, answers to the following questions remained inconclusive: (1) the cause and commencement timing of the evaporitic deposition and (2) when and what resulted in the shift of evaporitic deposition to a playa environment. A deep paleo-lake prior to the evaporite deposit formation, as hypothesized by previous studies, is proven unlikely by increasing evidence from sedimentologic and geomorphic studies. Bieletan, the westernmost sub-playa of Qarhan today, did not belong to the uniform Qarhan Salt Flat until the beginning of the deposition of the top 20-m evaporitic sequence, based on both the configuration of evaporitic strata and the distribution pattern of the lithium deposit. -
United States Patent (11) 3,615,174
United States Patent (11) 3,615,174 72 Inventor William J. Lewis 3,342,548 9/1967 Macey....... A. 2319 X South Ogden, Utah 3,432,031 3/1969 Ferris........................... 209/166 X 21 Appl. No. 740,886 FOREIGN PATENTS 22, Filed June 28, 1968 45 Patented Oct. 26, 1971 1,075,166 4f1954 France ......................... 209/66 (73) Assignee NL Industries, Inc. OTHER REFERENCES New York, N.Y. Chem. Abst., Vol. 53, 1959, 9587e I & EC, Vol. 56, 7, Jy '64, 61 & 62. Primary Examiner-Frank W. Lutter 54 PROCESSFOR THE SELECTIVE RECOVERY OF Assistant Examiner-Robert Halper POTASSUMAND MAGNESUMWALUES FROM Attorney-Ward, McElhannon, Brooks & Fitzpatrick AQUEOUSSALT SOLUTIONS CONTAINING THE SAME 11 Claims, 4 Drawing Figs. ABSTRACT: Kainite immersed in brine in equilibrium con 52) U.S. Cl........................................................ 23138, verted to carnalite by cooling to about 10 C. or under. Car 209/11, 209/166,23191, 22/121 nallite so obtained purified by cold flotation. Purified carnal (5) Int. Cl......................................................... B03b 1100, lite water leached to yield magnesium chloride brine and B03d 1102, C01f 5126 potassium chloride salt. Latter optionally converted to potas 50 Field of Search............................................ 209/166,3, sium sulfate by reaction with kainite, or by reacting the carnal 10, 11; 23.19, 38, 121 lite with kainite. Naturally occurring brine concentrated to precipitate principally sodium chloride, mother liquor warm 56 References Cited concentrated to precipitate kainite, cooled under mother UNITED STATES PATENTS liquor for conversion to carnallite. A crude kainite fraction 2,479,001 8/1949 Burke........................... 23.191 purified by warm flotation and a crude carnallite fraction pu 2,689,649 9, 1954 Atwood.... -
OCCURRENCE of BROMINE in CARNALLITE and SYLVITE from UTAH and NEW MEXICO* Manrr Loursp Lrnosonc
OCCURRENCE OF BROMINE IN CARNALLITE AND SYLVITE FROM UTAH AND NEW MEXICO* Manrr Loursp LrNosonc ABSTRACT Both carnallite and sylvite from Eddy County, New Mexico, contain 0.1 per cent of bromine. The bromine content of these minerals from Grand county, utah, is three times as great. No bromine was detected in halite, polyhalite, l5ngbeinite, or anhydrite from New Mexico. Iodine was not detected in any of these minerals. on the basis of the bromine content of the sylvite from New Mexico, it is calculated that 7,000 tons of bromine were present in potash salts mined from the permian basin during the period 1931 to 1945. INrnooucrroN The Geological Survey has previously made tests for bromine and iodine in core samples of potash salts from New Mexico.r Bromine was found to be present in very small amounts. No systematic quantitative determinations were made, nor was the presenceof bromine specificalry correlated with quantitative mineral composition. Sections of potash core from four recently drilled wells and selected pure saline minerals from Eddy County, New Mexico, together with two cores from Grand County, Utah, were therefore analyzed for their bromine and iodine content. The percentage mineral composition was then correlated with the bromine content. rt was found that bromine was restricted to carnall- ite and sylvite. fodine was not detected in any of the samples analyzed. If present, its quantity must be less than .00570. Brine and sea water are the present commercial sourcesof bromine in the United States, though both Germany and U.S.S.R. have utilized potash salts as a source of bromine. -
Lake Status Records from China: Data Base Documentation
Lake status records from China: Data Base Documentation G. Yu 1,2, S.P. Harrison 1, and B. Xue 2 1 Max Planck Institute for Biogeochemistry, Postfach 10 01 64, D-07701 Jena, Germany 2 Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences. Nanjing 210008, China MPI-BGC Tech Rep 4: Yu, Harrison and Xue, 2001 ii MPI-BGC Tech Rep 4: Yu, Harrison and Xue, 2001 Table of Contents Table of Contents ............................................................................................................ iii 1. Introduction ...............................................................................................................1 1.1. Lakes as Indicators of Past Climate Changes........................................................1 1.2. Chinese Lakes as Indicators of Asian Monsoonal Climate Changes ....................1 1.3. Previous Work on Palaeohydrological Changes in China.....................................3 1.4. Data and Methods .................................................................................................6 1.4.1. The Data Set..................................................................................................6 1.4.2. Sources of Evidence for Changes in Lake Status..........................................7 1.4.3. Standardisation: Lake Status Coding ..........................................................11 1.4.4. Chronology and Dating Control..................................................................11 1.5. Structure of this Report .......................................................................................13 -
Anomalously High Cretaceous Paleobrine Temperatures: Hothouse, Hydrothermal Or Solar Heating?
minerals Article Anomalously High Cretaceous Paleobrine Temperatures: Hothouse, Hydrothermal or Solar Heating? Jiuyi Wang 1,2 ID and Tim K. Lowenstein 2,* 1 MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China; [email protected] 2 Department of Geological Sciences and Environmental Studies, State University of New York, Binghamton, NY 13902, USA * Correspondence: [email protected]; Tel.: +1-607-777-4254 Received: 1 November 2017; Accepted: 9 December 2017; Published: 13 December 2017 Abstract: Elevated surface paleobrine temperatures (average 85.6 ◦C) are reported here from Cretaceous marine halites in the Maha Sarakham Formation, Khorat Plateau, Thailand. Fluid inclusions in primary subaqueous “chevron” and “cumulate” halites associated with potash salts contain daughter crystals of sylvite (KCl) and carnallite (MgCl2·KCl·6H2O). Petrographic textures demonstrate that these fluid inclusions were trapped from the warm brines in which the halite crystallized. Later cooling produced supersaturated conditions leading to the precipitation of sylvite and carnallite daughter crystals within fluid inclusions. Dissolution temperatures of daughter crystals in fluid inclusions from the same halite bed vary over a large range (57.9 ◦C to 117.2 ◦C), suggesting that halite grew at different temperatures within and at the bottom of the water column. Consistency of daughter crystal dissolution temperatures within fluid inclusion bands and the absence of vapor bubbles at room temperature demonstrate that fluid inclusions have not stretched or leaked. Daughter crystal dissolution temperatures are reproducible to within 0.1 ◦C to 10.2 ◦C (average of 1.8 ◦C), and thus faithfully document paleobrine conditions. -
Potash Deposits in the Devonian Prairie Evaporite, Southwestern Manitoba Lo Eo Gic G a a L B S O U
Potash deposits in the Devonian Prairie Evaporite, southwestern Manitoba lo eo gic g a a l b s o u t r i v n e a MGS y m M.P.B. Nicolas 1928 Manitoba Geological Survey, Winnipeg, Manitoba, Canada Potash Geology 3. Esterhazy Member The Esterhazy Member is the most economic Potash Exploration potash beds. It consists of euhedral to subhedal halite 2. Regional and Local Geology crystals with large anhedral sylvite crystals and minor 1. Introduction interstitial carnolite and clays (Figure 7 and 8). In Manitoba, the Paleozoic-, Mesozoic- and Cenozoic-age strata form a basinward-thickening, southwesterly- 6. Potash Resource 7. Exploration History The Prairie Evaporite is a thick Denonian-aged evaporitic sloping wedge, with the strata reaching a total thickness of 2.3 km in the extreme southestern corner of Manitoba The Esterhazy Member is intermittently present in R29W1 R28 R27 R26 R25 R24 R23 sequence dominantly consisting of halite and anhydrite. It Legend (Figure 4). The potash-bearing Devonian-age Prairie Evaporite was deposited within the Elk Point Basin (Figure Formal mineral resource estimates have been prepared for The discovery of potash in Manitoba was in an oil well T30 a narrow, elongate strip in southwestern Manitoba, includes four potash-bearing members, from oldest to youngest N 5). The Prairie Evaporite consists mainly of thick halite beds, with minor anhydrite and four localized potash beds. the Russell deposit, most recently in 2009. A historical resource drilled in 1951 at 15-18-10-27W1. This discovery led to salt distribution WA T29 from Township 5 to 21, Ranges 27 to 29 W1 (Figure E A H B C Within the basin, the formation can exceed 210 m in thickness, and lies at depths of 200 to 2,700 m below surface. -
Assessment of the Molecular Structure of the Borate Mineral Boracite
Spectrochimica Acta Part A: Molecular and Biomolecular Spectroscopy 96 (2012) 946–951 Contents lists available at SciVerse ScienceDirect Spectrochimica Acta Part A: Molecular and Biomolecular Spectroscopy journal homepage: www.elsevier.com/locate/saa Assessment of the molecular structure of the borate mineral boracite Mg3B7O13Cl using vibrational spectroscopy ⇑ Ray L. Frost a, , Yunfei Xi a, Ricardo Scholz b a School of Chemistry, Physics and Mechanical Engineering, Science and Engineering Faculty, Queensland University of Technology, G.P.O. Box 2434, Brisbane, Queensland 4001, Australia b Geology Department, School of Mines, Federal University of Ouro Preto, Campus Morro do Cruzeiro, Ouro Preto, MG 35400-00, Brazil highlights graphical abstract " Boracite is a magnesium borate mineral with formula: Mg3B7O13Cl. " The crystals belong to the orthorhombic – pyramidal crystal system. " The molecular structure of the mineral has been assessed. " Raman spectrum shows that some Cl anions have been replaced with OH units. article info abstract Article history: Boracite is a magnesium borate mineral with formula: Mg3B7O13Cl and occurs as blue green, colorless, Received 23 May 2012 gray, yellow to white crystals in the orthorhombic – pyramidal crystal system. An intense Raman band Received in revised form 2 July 2012 À1 at 1009 cm was assigned to the BO stretching vibration of the B7O13 units. Raman bands at 1121, Accepted 9 July 2012 1136, 1143 cmÀ1 are attributed to the in-plane bending vibrations of trigonal boron. Four sharp Raman Available online 13 August 2012 bands observed at 415, 494, 621 and 671 cmÀ1 are simply defined as trigonal and tetrahedral borate bending modes. The Raman spectrum clearly shows intense Raman bands at 3405 and 3494 cmÀ1, thus Keywords: indicating that some Cl anions have been replaced with OH units. -
Minerals Found in Michigan Listed by County
Michigan Minerals Listed by Mineral Name Based on MI DEQ GSD Bulletin 6 “Mineralogy of Michigan” Actinolite, Dickinson, Gogebic, Gratiot, and Anthonyite, Houghton County Marquette counties Anthophyllite, Dickinson, and Marquette counties Aegirinaugite, Marquette County Antigorite, Dickinson, and Marquette counties Aegirine, Marquette County Apatite, Baraga, Dickinson, Houghton, Iron, Albite, Dickinson, Gratiot, Houghton, Keweenaw, Kalkaska, Keweenaw, Marquette, and Monroe and Marquette counties counties Algodonite, Baraga, Houghton, Keweenaw, and Aphrosiderite, Gogebic, Iron, and Marquette Ontonagon counties counties Allanite, Gogebic, Iron, and Marquette counties Apophyllite, Houghton, and Keweenaw counties Almandite, Dickinson, Keweenaw, and Marquette Aragonite, Gogebic, Iron, Jackson, Marquette, and counties Monroe counties Alunite, Iron County Arsenopyrite, Marquette, and Menominee counties Analcite, Houghton, Keweenaw, and Ontonagon counties Atacamite, Houghton, Keweenaw, and Ontonagon counties Anatase, Gratiot, Houghton, Keweenaw, Marquette, and Ontonagon counties Augite, Dickinson, Genesee, Gratiot, Houghton, Iron, Keweenaw, Marquette, and Ontonagon counties Andalusite, Iron, and Marquette counties Awarurite, Marquette County Andesine, Keweenaw County Axinite, Gogebic, and Marquette counties Andradite, Dickinson County Azurite, Dickinson, Keweenaw, Marquette, and Anglesite, Marquette County Ontonagon counties Anhydrite, Bay, Berrien, Gratiot, Houghton, Babingtonite, Keweenaw County Isabella, Kalamazoo, Kent, Keweenaw, Macomb, Manistee, -
Experimental Drill Hole Logging in Potash Deposits Op the Cablsbad District, Hew Mexico
EXPERIMENTAL DRILL HOLE LOGGING IN POTASH DEPOSITS OP THE CABLSBAD DISTRICT, HEW MEXICO By C. L. Jones, C. G. Bovles, and K. G. Bell U. S. GEOLOGICAL SURVEY This report is preliminary and has not been edited or Released to open, files reviewed for conformity to Geological Survey standards or nomenclature. COHTEUTS Page Abstract i Introduction y 2 Geology . .. .. .....-*. k Equipment 7 Drill hole data . - ...... .... ..-. - 8 Supplementary tests 10 Gamma-ray logs -T 11 Grade and thidmess estimates from gamma-ray logs Ik Neutron logs 15 Electrical resistivity logs 18 Literature cited . ........... ........ 21 ILLUSTRATIONS Figure 1. Generalized columnar section and radioactivity log of potassium-bearing rocks 2. Abridged gamma-ray logs recorded by commercial All companies and the U. S. Geological Survey figures 3« Lithologic, gamma-ray, neutron, and electrical resistivity logs ................. are in k. Abridged gamma-ray and graphic logs of a potash envelope deposit at end of 5« Lithologic interpretations derived from gamma-ray and electrical resistivity logs - ...... report. TABLE Table 1. Summary of drill hole data 9 EXPERIMENTAL DRILL HOLE LOGGING Iff POTASH DEPOSITS OP THE CARISBAD DISTRICT, HEW MEXICO By C. L. Jones, C. G. Bowles, and K. G>. Bell ABSTRACT Experimental logging of holes drilled through potash deposits in the Carlsbad district, southeastern Hew Mexico, demonstrate the consider able utility of gamma-ray, neutron, and electrical resistivity logging in the search for and identification of mineable deposits of sylvite and langbeinite. Such deposits are strongly radioactive with both gamma-ray and neutron well logging. Their radioactivity serves to distinguish them from clay stone, sandstone, and polyhalite beds and from potash deposits containing carnallite, leonite, and kainite.