wanyu/IteraTeR_v2 huggingface dataset:
Original:  Occurrence and Paragenesis Georgeericksonite is commonly found as isolated bright lemon-yellow micronodules of crystals that are concentrated on the surface of one part of the mineral specimen.
Revised:  Occurrence and Paragenesis George-ericksonite is commonly found as isolated bright lemon-yellow micronodules of crystals that are concentrated on the surface of one part of the mineral specimen.
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Original:  Even at low currents and short counting times georgeericksenite is extremely unstable under the electron beam.
Revised:  Even at low currents and short counting times george-ericksenite is extremely unstable under the electron beam.
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Original:  The overall quantitative behavior of georgeericksenite in the electron beam is consistent with the chemical composition derived (ideally I2O5 59.13, CrO3 9.92. SO3 1.51, MgO 2.38, CaO 3.31, Na2O 10.98, H2O 12.77 weight \%).
Revised:  The overall quantitative behavior of george-ericksenite in the electron beam is consistent with the chemical composition derived (ideally I2O5 59.13, CrO3 9.92. SO3 1.51, MgO 2.38, CaO 3.31, Na2O 10.98, H2O 12.77 weight \%).
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Original:  The result was placing georgeericksenite in the C2/c space group.
Revised:  The result was placing george-ericksenite in the C2/c space group.
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Original:  Structure Topology Georgeericksenite features a structural arrangement that is composed of slabs of polyhedra orthogonal to [100].
Revised:  Structure Topology George-ericksenite features a structural arrangement that is composed of slabs of polyhedra orthogonal to [100].
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Original:  Dietzeite and georgeericksenite have no structural relationship.
Revised:  Dietzeite and george-ericksenite have no structural relationship.
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Original:  They are also sheet structures, but the sheets are vastly different in terms of connectivity than in georgeericksenite .
Revised:  They are also sheet structures, but the sheets are vastly different in terms of connectivity than in george-ericksenite .
Edit intent: fluency
Original: Occurrence and Paragenesis George-ericksonite is commonly found as isolated bright lemon-yellow micronodules of crystals that are concentrated on the surface of one part of the mineral specimen.
Revised: Occurrence and paragenesis George-ericksonite is commonly found as isolated bright lemon-yellow micronodules of crystals that are concentrated on the surface of one part of the mineral specimen.
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Original:  Electron Microprobe Examination This examination was carried out by attaching two acicular crystals to the surface of a disk with epoxy and then examining them with a CAMECA SX-50 electron microprobe.
Revised:  Electron microprobe examination This examination was carried out by attaching two acicular crystals to the surface of a disk with epoxy and then examining them with a CAMECA SX-50 electron microprobe.
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Original:  Crystal Structure Data Collection A 0.046 X 0.059 X 0.060 mm3 crystal was mounted on a Siemans P4 four-circle diffractometer.
Revised:  Crystal structure Data Collection A 0.046 X 0.059 X 0.060 mm3 crystal was mounted on a Siemans P4 four-circle diffractometer.
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Original:  Crystal Structure Data Collection A 0.046 X 0.059 X 0.060 mm3 crystal was mounted on a Siemans P4 four-circle diffractometer.
Revised:  Crystal Structure Data collection A 0.046 X 0.059 X 0.060 mm3 crystal was mounted on a Siemans P4 four-circle diffractometer.
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Original:  Structure Solution and Refinement The SHELXTL PC Plus system of programs were used for the calculations.
Revised:  Structure solution and refinement The SHELXTL PC Plus system of programs were used for the calculations.
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Original:  Description of the Structure Cation Coordination There is one chromium (Cr) site that is symmetrically distinct and is tetrahedrally coordinated by four oxygen (O) atoms.
Revised:  Description of the structure Cation Coordination There is one chromium (Cr) site that is symmetrically distinct and is tetrahedrally coordinated by four oxygen (O) atoms.
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Original:  Description of the Structure Cation Coordination There is one chromium (Cr) site that is symmetrically distinct and is tetrahedrally coordinated by four oxygen (O) atoms.
Revised:  Description of the Structure Cation coordination There is one chromium (Cr) site that is symmetrically distinct and is tetrahedrally coordinated by four oxygen (O) atoms.
Edit intent: fluency
Original:  Structure Topology George-ericksenite features a structural arrangement that is composed of slabs of polyhedra orthogonal to [100].
Revised:  Structure topology George-ericksenite features a structural arrangement that is composed of slabs of polyhedra orthogonal to [100].
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Original:  Relation to Other Minerals The only other chromate-iodate mineral is dietzeite, Ca(IO3)2(CrO4)(H2O).
Revised:  Relation to other minerals The only other chromate-iodate mineral is dietzeite, Ca(IO3)2(CrO4)(H2O).
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Original:  The R and Rw indicies are of the conventional form.
Revised:  The R and Rw indices are of the conventional form.
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Original:  The layers stack in an ABAB fashion along the c, there is no obvious eutaxy, they can be described as chains of corner-sharing LiO4 tetrahedra cross connected by PO3F tetrahedra  
Revised:  The layers stack in an ABAB fashion along the c, there is no obvious eutaxy, they can be described as chains of corner-sharing LiO4 tetrahedra cross connected by PO3F tetrahedra . 
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Original:  Relationship of Bobdownsite to other Species Member of: Whitlockite Group Other Members of Group : FerromerrilliteCa9NaFe2+(PO4)7Hedegaardite(Ca,Na)9(Ca,Na)Mg(PO4)6(PO3OH)MerrilliteCa9NaMg(PO4)7StrontiowhitlockiteSr9Mg(PO4)6(HPO4)TuiteCa3(PO4)2WhitlockiteCa9Mg(PO4)6(HPO4) Geological occurrences Tait, Kimberly T.,Madison C. Barkley, Richard M.
Revised:  Relationship of bobdownsite to other species Member of: Whitlockite Group Other Members of Group : FerromerrilliteCa9NaFe2+(PO4)7Hedegaardite(Ca,Na)9(Ca,Na)Mg(PO4)6(PO3OH)MerrilliteCa9NaMg(PO4)7StrontiowhitlockiteSr9Mg(PO4)6(HPO4)TuiteCa3(PO4)2WhitlockiteCa9Mg(PO4)6(HPO4) Geological occurrences Tait, Kimberly T.,Madison C. Barkley, Richard M.
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Original:  Relationship of Bobdownsite to other Species Member of: Whitlockite Group Other Members of Group : FerromerrilliteCa9NaFe2+(PO4)7Hedegaardite(Ca,Na)9(Ca,Na)Mg(PO4)6(PO3OH)MerrilliteCa9NaMg(PO4)7StrontiowhitlockiteSr9Mg(PO4)6(HPO4)TuiteCa3(PO4)2WhitlockiteCa9Mg(PO4)6(HPO4) Geological occurrences Tait, Kimberly T.,Madison C. Barkley, Richard M.
Revised:  Relationship of Bobdownsite to other Species Member of: whitlockite group Other Members of Group : FerromerrilliteCa9NaFe2+(PO4)7Hedegaardite(Ca,Na)9(Ca,Na)Mg(PO4)6(PO3OH)MerrilliteCa9NaMg(PO4)7StrontiowhitlockiteSr9Mg(PO4)6(HPO4)TuiteCa3(PO4)2WhitlockiteCa9Mg(PO4)6(HPO4) Geological occurrences Tait, Kimberly T.,Madison C. Barkley, Richard M.
Edit intent: fluency
Original:  Relationship of Bobdownsite to other Species Member of: Whitlockite Group Other Members of Group : FerromerrilliteCa9NaFe2+(PO4)7Hedegaardite(Ca,Na)9(Ca,Na)Mg(PO4)6(PO3OH)MerrilliteCa9NaMg(PO4)7StrontiowhitlockiteSr9Mg(PO4)6(HPO4)TuiteCa3(PO4)2WhitlockiteCa9Mg(PO4)6(HPO4) Geological occurrences Tait, Kimberly T.,Madison C. Barkley, Richard M.
Revised:  Relationship of Bobdownsite to other Species Member of: Whitlockite Group Other members of group : FerromerrilliteCa9NaFe2+(PO4)7Hedegaardite(Ca,Na)9(Ca,Na)Mg(PO4)6(PO3OH)MerrilliteCa9NaMg(PO4)7StrontiowhitlockiteSr9Mg(PO4)6(HPO4)TuiteCa3(PO4)2WhitlockiteCa9Mg(PO4)6(HPO4) Geological occurrences Tait, Kimberly T.,Madison C. Barkley, Richard M.
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Original:   Physical Properties Bobdownsite is an naturally forming P-F phosphate mineral found in two terrestrial locations: Tip Top mine, South Dakota, and Big Fish River, Yukon, Canada.
Revised:  Physical properties Bobdownsite is an naturally forming P-F phosphate mineral found in two terrestrial locations: Tip Top mine, South Dakota, and Big Fish River, Yukon, Canada.
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Original:  The layers stack in an ABAB fashion along the c, there is no obvious eutaxy, they can be described as chains of corner-sharing LiO4 tetrahedra cross connected by PO3F tetrahedra . Composition Sodium 0.52 \% Na 0.71 \% Na2OCalcium 33.30 \% Ca 46.59 \% CaOMagnesium 1.66 \% Mg 2.75 \% MgOAluminum 0.28 \% Al 0.53 \% Al2O3Iron 0.90 \% Fe 0.27 \% FeO / 0.98 \% Fe2O3Phosphorus 20.56 \% P 47.12 \% P2O5Oxygen 40.97 \% OFluorine 1.80 \% F 1.80 \% F -
Revised:  The layers stack in an ABAB fashion along the c, there is no obvious eutaxy, they can be described as chains of corner-sharing LiO4 tetrahedra cross connected by PO3F tetrahedra Composition Sodium 0.52 \% Na 0.71 \% Na2OCalcium 33.30 \% Ca 46.59 \% CaOMagnesium 1.66 \% Mg 2.75 \% MgOAluminum 0.28 \% Al 0.53 \% Al2O3Iron 0.90 \% Fe 0.27 \% FeO / 0.98 \% Fe2O3Phosphorus 20.56 \% P 47.12 \% P2O5Oxygen 40.97 \% OFluorine 1.80 \% F 1.80 \% F -
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Original:  Bobdownsite is named after Dr. Robert Terrace Downs a professor of mineralogy in the Department of Geosciences at the University of Arizona, of whom lived and worked in the Yukon Territory in the 1970s .
Revised:  Bobdownsite is named after Robert Terrace Downs a professor of mineralogy in the Department of Geosciences at the University of Arizona, of whom lived and worked in the Yukon Territory in the 1970s .
Edit intent: coherence
Original:  Bobdownsite is named after Dr. Robert Terrace Downs a professor of mineralogy in the Department of Geosciences at the University of Arizona, of whom lived and worked in the Yukon Territory in the 1970s .
Revised:  Bobdownsite is named after Dr. Robert Terrace Downs a professor of mineralogy in the Department of Geosciences at the University of Arizona, who lived and worked in the Yukon Territory in the 1970s .
Edit intent: coherence
Original:  Samples recovered from this exposure are  Lower Cretaceous bedded ironstones and shales.
Revised:  Samples recovered from this exposure are found with Lower Cretaceous bedded ironstones and shales.
Edit intent: clarity
Original:  Bobdownsite is a phosphatic mineral with its exposure downstream from phosphatic nodule slopes.
Revised:  Bobdownsite is a phosphate mineral with its exposure downstream from phosphatic nodule slopes.
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Original:  Bobdownsite is a phosphatic mineral with its exposure downstream from phosphatic nodule slopes.
Revised:  Bobdownsite is a phosphatic mineral with its exposure downstream from phosphate nodule slopes.
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Original:  It occurs next to siderite, lazulite, kulanite, gormanite, quartz , and collinsite.
Revised:  It occurs associated with siderite, lazulite, kulanite, gormanite, quartz , and collinsite.
Edit intent: clarity
Original:  It occurs next to siderite, lazulite, kulanite, gormanite, quartz , and collinsite.
Revised:  It occurs next to siderite, lazulite, kulanite, gormanite, quartz and collinsite.
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Original:  But bobdownsite is also located in the Tip Top mine of Custer County, South Dakota.
Revised:  Bobdownsite has also been reported from the Tip Top mine of Custer County, South Dakota.
Edit intent: clarity
Original:  Further more it has been found with other witlockite group minerals in Martian meteorites.
Revised:  Furthermore it has been found with other witlockite group minerals in Martian meteorites.
Edit intent: coherence
Original:  Thompson, Marcus J. Origlieri, Stanley H. Evans, Charles T. Prewitt, and Hexiong Yang, "Bobdownsite, A New Mineral SPecies From Big FIsh River, Yukon, Canada, and Its Structural Relationship With Whitlockite-Type Compounds"  49.4 (2011): (1065-1078).
Revised:  Thompson, Marcus J. Origlieri, Stanley H. Evans, Charles T. Prewitt, and Hexiong Yang, "Bobdownsite, A New Mineral Species From Big FIsh River, Yukon, Canada, and Its Structural Relationship With Whitlockite-Type Compounds" 49.4 (2011): (1065-1078).
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Original:  Print. Meteorites Bobdownsite, whitlockite, and merrillite are all important phosphate minerals found  in lunar rocks and closely related .
Revised:  Print. Meteorites Bobdownsite, whitlockite, and merrillite are all important phosphate minerals found closely related in lunar rocks and closely related .
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Original:  Print. Meteorites Bobdownsite, whitlockite, and merrillite are all important phosphate minerals found  in lunar rocks and closely related .
Revised:  Print. Meteorites Bobdownsite, whitlockite, and merrillite are all important phosphate minerals found in lunar rocks .
Edit intent: coherence
Original:  Merrillite crystals with considerable amounts of F and traces of Cl were found in several martian meteorites.
Revised:  Merrillite crystals with considerable amounts of F and traces of chlorine were found in several martian meteorites.
Edit intent: clarity
Original:  Merrillite crystals with considerable amounts of F and traces of Cl were found in several martian meteorites.
Revised:  Merrillite crystals with considerable amounts of F and traces of Cl were found in several Martian meteorites.
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Original:  In Yukon, Canada bobdownsite is found composed of anhedral and euhedral crystals, tabular, colorless in transmitted light, transparent,  a white streak and a vitreous luster.
Revised:  In Yukon, Canada bobdownsite is found composed of anhedral and euhedral crystals, tabular, colorless in transmitted light, transparent, with a white streak and a vitreous luster.
Edit intent: coherence
Original:  The point group is 3m with unit cell parameters ɑ 1.3224(3)  , c 37.70(2) Å, V 3420.7(6) Å³. Bobdownsite has trigonal - ditrigonal pyramid tabular, euhedral crystals.
Revised:  The point group is 3m with unit cell parameters ɑ 1.3224(3) Å , c 37.70(2) Å, V 3420.7(6) Å³. Bobdownsite has trigonal - ditrigonal pyramid tabular, euhedral crystals.
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Original:  The octahedral sites contain PO3F tetrahedral groups which are approximately in the midplane between the two pinwheel layers and are each coordinated to the closest two interlayer Ca cations by the Oxygen .
Revised:  The octahedral sites contain PO3F tetrahedral groups which are approximately in the midplane between the two pinwheel layers and are each coordinated to the closest two interlayer Ca cations by the oxygen .
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Original: Bobdownsite is the fluorine-dominated mineral of the whitlockite group of phosphate minerals whose formula is Ca9(Mg)(PO4)6(PO3F).
Revised: Bobdownsite is the fluorine bearing mineral of the whitlockite group of phosphate minerals whose formula is Ca9(Mg)(PO4)6(PO3F).
Edit intent: clarity
Original:  Bobdownsite occurs in a vein from a east- west- trending faulted vein.
Revised:  Bobdownsite occurs in a vein from an east- west- trending faulted vein.
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Original:  Furthermore  it has been found with other witlockite group minerals in Martian meteorites.
Revised:  Furthermore , it has been found with other witlockite group minerals in Martian meteorites.
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Original: Bobdownsite is the fluorine bearing mineral of the whitlockite group of phosphate minerals whose formula is Ca9(Mg)(PO4)6(PO3F).
Revised: Bobdownsite is the fluorine-bearing mineral of the whitlockite group of phosphate minerals whose formula is Ca9(Mg)(PO4)6(PO3F).
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Original:  Implications for geochronology and low-temperature processes, Chemical Geology, Volume 254, Issues 3–4, 15 September 2008, Pages 238-248 in Chemical Geology] [J.R. Dooley, Jr., and John C. Hathaway, 1961, Two Occurences of Thorium-bearing Minerals with Rhabdophane-like Structures, USGS Professional Paper 424-C, pg. 339-341] As Member of Rhabdophane Group Grayite is isostructural with members of the Rhabdophane group such as brockite and rhabdrophane.
Revised:  Implications for geochronology and low-temperature processes, Chemical Geology, Volume 254, Issues 3–4, 15 September 2008, Pages 238-248 in Chemical Geology] [J.R. Dooley, Jr., and John C. Hathaway, 1961, Two Occurences of Thorium-bearing Minerals with Rhabdophane-like Structures, USGS Professional Paper 424-C, pg. 339-341] As Member of rhabdophane group Grayite is isostructural with members of the Rhabdophane group such as brockite and rhabdrophane.
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Original:  Relationship with Monazite In the identification of new hydrated phosphate minerals related to rhabdophane XRD peak information is usually recorded through different sample preparation methods.
Revised:  Relationship with monazite In the identification of new hydrated phosphate minerals related to rhabdophane XRD peak information is usually recorded through different sample preparation methods.
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Original:  Grayite has often been found in pegmatitic environments amongst other thorium minerals, particularly monazite ( (Ce,La)PO4 ).
Revised:  Grayite has often been found in pegmatitic environments amongst other thorium minerals, particularly monazite ( ).
Edit intent: coherence
Original: Grayite, ThPO4 • (H2O), is a thorium phosphate mineral of the Rabdophane group first discovered in 1957 by S.H.U. Bowie in Rhodesia.
Revised: Grayite, ThPO4 · (H2O), is a thorium phosphate mineral of the Rabdophane group first discovered in 1957 by S.H.U. Bowie in Rhodesia.
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Original:  It has a low to moderate hardness with a Mohs hardness of 3-4 and has a specific gravity of 3.7 -4.3 . It has been found in both intrusive igneous and sedimentary environments.
Revised:  It has a low to moderate hardness with a Mohs hardness of 3–4 and has a specific gravity of 3.7 -4.3 . It has been found in both intrusive igneous and sedimentary environments.
Edit intent: clarity
Original:  It has a low to moderate hardness with a Mohs hardness of 3-4 and has a specific gravity of 3.7 -4.3 . It has been found in both intrusive igneous and sedimentary environments.
Revised:  It has a low to moderate hardness with a Mohs hardness of 3-4 and has a specific gravity of 3.7 –4.3 . It has been found in both intrusive igneous and sedimentary environments.
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Original: Botswana educators Category:Botswana male writers Category:Botswana politicians Category:White South African people Category:Afrikaner people Category:South African people of Dutch descent Category:South African diplomats Category:South African exiles Category:South African expatriates in the United Kingdom Category:South African Roman Catholics Category:Anti-apartheid activists Category:Botswana non-fiction writers Category:Botswana journalists Category:Male journalis 
Revised: Botswana educators Category:Botswana male writers Category:Botswana politicians Category:White South African people Category:Afrikaner people Category:South African people of Dutch descent Category:South African diplomats Category:South African exiles Category:South African expatriates in the United Kingdom Category:South African Roman Catholics Category:Anti-apartheid activists Category:Botswana non-fiction writers Category:Botswana journalists Category:Male journalists 
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Original: The Hurmuzachi brothers, Alexandru (1823-1871), Constantin (1811-1869), Eudoxiu (1812-1874), Gheorghe (1817-1882), and Nicolae (1826-1909) were members of an old Hurmuzachi family of Romanian nobles in Austrian Bukovina of Greek origin, with their estate in Cernauca.
Revised: The Hurmuzachi brothers, Alexandru (1823-1871), Constantin (1811-1869), Eudoxiu (1812-1874), Gheorghe (1817-1882), and Nicolae (1826-1909) were members of an old Hurmuzachi family of Romanian nobles in Austrian BukovinaChastain of Greek origin, with their estate in Cernauca.
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Original: The Hurmuzachi brothers, Alexandru (1823-1871), Constantin (1811-1869), Eudoxiu (1812-1874), Gheorghe (1817-1882), and Nicolae (1826-1909) were members of an old Hurmuzachi family of Romanian nobles in Austrian Bukovina of Greek origin, with their estate in Cernauca.
Revised: The Hurmuzachi brothers, Alexandru (1823-1871), Constantin (1811-1869), Eudoxiu (1812-1874), Gheorghe (1817-1882), and Nicolae (1826-1909) were members of an old Hurmuzachi family of Romanian nobles in Austrian Bukovina of Greek origin, with an estate in Cernauca.
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Original:   Their   father was Doxachi (Doxache, Doxaki) Hurmuzachi (Hurmuzaki).
Revised:  Their Their father was Doxachi (Doxache, Doxaki) Hurmuzachi (Hurmuzaki).
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Original:   Alexandru Hurmuzachi was the honorary member of the Romanian Academy.
Revised:  Eudoxiu and Alexandru Hurmuzachi were members of the Romanian Academy.
Edit intent: clarity
Original: The Hurmuzachi brothers, Alexandru (1823-1871), Constantin (1811-1869), Eudoxiu (1812-1874), Gheorghe (1817-1882), and Nicolae (1826-1909), were members of an old Hurmuzachi family of Romanian nobles in Austrian BukovinaChastain of Greek origin, with an estate in Cernăuca.
Revised: The Hurmuzachi brothers, Alexandru (1823-1871), Constantin (1811-1869), Eudoxiu (1812-1874), Gheorghe (1817-1882), and Nicolae (1826-1909), were members of an old Hurmuzachi family of Romanian nobles in Austrian BukovinaChastain with an estate in Cernăuca.
Edit intent: coherence
Original:  See here for a table detailing the elements of celestial coordinate systems, including each's primary direction
Edit intent: clarity
Original:  The Supreme Junta (or Junta Suprema de Caracas) was the institution that governed the Captaincy General of Venezuela following the forced resignation of the Captain General Vicente Emparan on April 19, 1810, marking the beginning of the Venezuelan War of Independence.
Revised:  The Supreme Junta (or Junta Suprema de Caracas) was the institution that governed the Captaincy General of Venezuela following the forced resignation of the Captain General Vicente Emparán on April 19, 1810, marking the beginning of the Venezuelan War of Independence.
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Original: One of the first measures of revolutionaries after securing the support of six provinces  was to send diplomatic missions abroad to seek support for the revolution and the recognition of the Supreme Junta of Caracas as the legitimate councilor of Venezuela in the absence of the King.
Revised: One of the first measures taken by the revolutionaries, after securing the support of six provinces was to send diplomatic missions abroad to seek support for the revolution and the recognition of the Supreme Junta of Caracas as the legitimate councilor of Venezuela in the absence of the King.
Edit intent: clarity
Original: One of the first measures of revolutionaries after securing the support of six provinces  was to send diplomatic missions abroad to seek support for the revolution and the recognition of the Supreme Junta of Caracas as the legitimate councilor of Venezuela in the absence of the King.
Revised: One of the first measures of revolutionaries after securing the support of six provinces , was to send diplomatic missions abroad to seek support for the revolution and the recognition of the Supreme Junta of Caracas as the legitimate councilor of Venezuela in the absence of the King.
Edit intent: fluency
Original: One of the first measures of revolutionaries after securing the support of six provinces  was to send diplomatic missions abroad to seek support for the revolution and the recognition of the Supreme Junta of Caracas as the legitimate councilor of Venezuela in the absence of the King.
Revised: One of the first measures of revolutionaries after securing the support of six provinces was to send diplomatic missions abroad with the hope of gaining support and recognition for the revolution and the recognition of the Supreme Junta of Caracas as the legitimate councilor of Venezuela in the absence of the King.
Edit intent: clarity