wanyu/IteraTeR_v2 huggingface dataset:
Original:  The sinking of the basin follows the strong geometrical rule : the tectonic bloc, which carry the basin, is rotating around the straight line parallel to the water surface, and located onshore ( M ). As a result until the moment of main tectonic disturbance all borders of the layers remain flat and the geometrical inter-relations are described as perspective correspomdence.
Revised:  The sinking of the basin follows the strong geometrical restrictions : the tectonic bloc, which carry the basin, is rotating around the straight line parallel to the water surface, and located onshore ( M ). As a result until the moment of main tectonic disturbance all borders of the layers remain flat and the geometrical inter-relations are described as perspective correspomdence.
Edit intent: clarity
Original:  It means that if in three wells are known the thicknesses of layers belonging to the same stratigraphic unit  , then the thicknesses of these layers can be calculated for any location in the basin.
Revised:  It means that if in three wells the thicknesses of layers belonging to the same stratigraphic unit , then the thicknesses of these layers can be calculated for any location in the basin.
Edit intent: clarity
Original:  It means that if in three wells are known the thicknesses of layers belonging to the same stratigraphic unit  , then the thicknesses of these layers can be calculated for any location in the basin.
Revised:  It means that if in three wells are known the thicknesses of layers belonging to the same stratigraphic unit are known , then the thicknesses of these layers can be calculated for any location in the basin.
Edit intent: clarity
Original:  The most noticeable feature of the rocks, which filled the basins, is layering (stratification)  "stratification | geology".
Revised:  The most noticeable feature of the rocks, which filled the basins, is layering (stratification) . "stratification | geology".
Edit intent: fluency
Original:  Encyclopedia Britannica. . Stratigraphy is a part of Geology that investigates the phenomenon of layering.
Revised:  Encyclopedia Britannica. Stratigraphy is a part of Geology that investigates the phenomenon of layering.
Edit intent: fluency
Original:  Units are defined on the basis of their lithology and have no clear definitionChapter 5. Lithostratigraphic Units".
Revised:  Units are defined on the basis of their lithology and have no clear definition.Chapter 5. Lithostratigraphic Units".
Edit intent: fluency
Original:  2013–2014. . Geological Perspective Correlation (GPC) is a theory that divided the geological cross-section in units according strong mathematical rule: all borders of layers in this unit obey the law of perspective geometry  Young, John Wesley (1930), Projective Geometry, The Carus Mathematical Monographs (#4), Mathematical Association of America .
Revised:  2013–2014. Geological Perspective Correlation (GPC) is a theory that divided the geological cross-section in units according strong mathematical rule: all borders of layers in this unit obey the law of perspective geometry Young, John Wesley (1930), Projective Geometry, The Carus Mathematical Monographs (#4), Mathematical Association of America .
Edit intent: fluency
Original:  2013–2014. . Geological Perspective Correlation (GPC) is a theory that divided the geological cross-section in units according strong mathematical rule: all borders of layers in this unit obey the law of perspective geometry  Young, John Wesley (1930), Projective Geometry, The Carus Mathematical Monographs (#4), Mathematical Association of America .
Revised:  2013–2014. . Geological Perspective Correlation (GPC) is a theory that divided the geological cross-section in units according strong mathematical rule: all borders of layers in this unit obey the law of perspective geometry . Young, John Wesley (1930), Projective Geometry, The Carus Mathematical Monographs (#4), Mathematical Association of America .
Edit intent: fluency
Original:  2013–2014. . Geological Perspective Correlation (GPC) is a theory that divided the geological cross-section in units according strong mathematical rule: all borders of layers in this unit obey the law of perspective geometry  Young, John Wesley (1930), Projective Geometry, The Carus Mathematical Monographs (#4), Mathematical Association of America .
Revised:  2013–2014. . Geological Perspective Correlation (GPC) is a theory that divided the geological cross-section in units according strong mathematical rule: all borders of layers in this unit obey the law of perspective geometry Young, John Wesley (1930), Projective Geometry, The Carus Mathematical Monographs (#4), Mathematical Association of America 
Edit intent: fluency
Original:  As new layers are deposited the old ones are sinking deeper due to the weight of accumulating sedimentsAllen , Philip A.;
Revised:  As new layers are deposited the old ones are sinking deeper due to the weight of accumulating sediments.Allen , Philip A.;
Edit intent: fluency
Original:  Malden, MA [u.a.]: Blackwell. . The content of sedimentary layers (lithological and biological), their order in the sequence, and geometrical characteristics keep records of the history of the Earth, of past climate, sea-level and environment.
Revised:  Malden, MA [u.a.]: Blackwell. The content of sedimentary layers (lithological and biological), their order in the sequence, and geometrical characteristics keep records of the history of the Earth, of past climate, sea-level and environment.
Edit intent: fluency
Original:  the geological correlation problemVan Wagoner J., Mitchum R., Campion, K. and Rahmanian V. Siliciclastic Sequence Stratigraphy in Well Logs, Cores, and Outcrops: Concepts for High-Resolution Correlation of Time and Facies AAPG Methods in Exploration Series, No. 7, 1990. . The identification is based on comparison of 1) physical and mineralogical characteristics of the particular layer (lithostratigraphy), or 2) petrified remnants in this layer (biostratigraphy)  Kearey, Philip (2001).
Revised:  the geological correlation problemVan Wagoner J., Mitchum R., Campion, K. and Rahmanian V. Siliciclastic Sequence Stratigraphy in Well Logs, Cores, and Outcrops: Concepts for High-Resolution Correlation of Time and Facies AAPG Methods in Exploration Series, No. 7, 1990. The identification is based on comparison of 1) physical and mineralogical characteristics of the particular layer (lithostratigraphy), or 2) petrified remnants in this layer (biostratigraphy) Kearey, Philip (2001).
Edit intent: fluency
Original:  the geological correlation problemVan Wagoner J., Mitchum R., Campion, K. and Rahmanian V. Siliciclastic Sequence Stratigraphy in Well Logs, Cores, and Outcrops: Concepts for High-Resolution Correlation of Time and Facies AAPG Methods in Exploration Series, No. 7, 1990. . The identification is based on comparison of 1) physical and mineralogical characteristics of the particular layer (lithostratigraphy), or 2) petrified remnants in this layer (biostratigraphy)  Kearey, Philip (2001).
Revised:  the geological correlation problemVan Wagoner J., Mitchum R., Campion, K. and Rahmanian V. Siliciclastic Sequence Stratigraphy in Well Logs, Cores, and Outcrops: Concepts for High-Resolution Correlation of Time and Facies AAPG Methods in Exploration Series, No. 7, 1990. . The identification is based on comparison of 1) physical and mineralogical characteristics of the particular layer (lithostratigraphy), or 2) petrified remnants in this layer (biostratigraphy) . Kearey, Philip (2001).
Edit intent: fluency
Original:  Dictionary of Geology (2nd ed.) London, New York, etc.: Penguin Reference, London, p. 123.
Revised:  Dictionary of Geology (2nd ed.) London, New York, etc.: Penguin Reference, London, p. 123
Edit intent: fluency
Original:  This theory attracted attention around the world  , and particularly in Russia .
Revised:  This theory attracted attention around the world . , and particularly in Russia .
Edit intent: fluency
Original:  This theory attracted attention around the world  , and particularly in Russia .
Revised:  This theory attracted attention around the world , and particularly in Russia 
Edit intent: fluency
Original:  The theory is also a basis of the method of graphical correlation in biostratigraphy widely used in oil and coal industriesNemec W. (1988).
Revised:  The theory is also a basis of the method of graphical correlation in biostratigraphy widely used in oil and coal industries.Nemec W. (1988).
Edit intent: fluency
Original:  (eds.), New Perspectives in Basin Analysis © Springer-Verlag New York Inc. . Overview lang=en|upright=1.
Revised:  (eds.), New Perspectives in Basin Analysis © Springer-Verlag New York Inc. Overview lang=en|upright=1.
Edit intent: fluency
Original:  The ore geologists are looking for faults in the sediments – the ways, which deliver the melted mantle materials to the upper crustEvans A.
Revised:  The ore geologists are looking for faults in the sediments – the ways, which deliver the melted mantle materials to the upper crust.Evans A.
Edit intent: fluency
Original:  2005. Knowledge about underground geometry of the sedimentary basins comes from geological observations, geophysical measurements and from drillingFreudenrich C., Strickland J. How Oil Drilling Works.
Revised:  2005 Knowledge about underground geometry of the sedimentary basins comes from geological observations, geophysical measurements and from drillingFreudenrich C., Strickland J. How Oil Drilling Works.
Edit intent: fluency
Original:  2005. Knowledge about underground geometry of the sedimentary basins comes from geological observations, geophysical measurements and from drillingFreudenrich C., Strickland J. How Oil Drilling Works.
Revised:  2005. Knowledge about underground geometry of the sedimentary basins comes from geological observations, geophysical measurements and from drilling.Freudenrich C., Strickland J. How Oil Drilling Works.
Edit intent: fluency
Original:  It is natural that at the beginning of the exploration, when the number of wells is small, the correlation scheme contains expensive mistakesRandle C., Bond C., Lark M., Monaghan A. Can uncertainty in geological cross-section interpretations be quantified and predicted?
Revised:  It is natural that at the beginning of the exploration, when the number of wells is small, the correlation scheme contains expensive mistakes.Randle C., Bond C., Lark M., Monaghan A. Can uncertainty in geological cross-section interpretations be quantified and predicted?
Edit intent: fluency
Original:  This is why errors in correlation schemes are not seldom. . When the distances between available cross-sections are decreasing (for example, by drilling new wells) the quality of correlation is improving, but meanwhile the wrong geological decisions could be made that increases the expenses of geological projects.
Revised:  This is why errors in correlation schemes are not seldom. When the distances between available cross-sections are decreasing (for example, by drilling new wells) the quality of correlation is improving, but meanwhile the wrong geological decisions could be made that increases the expenses of geological projects.
Edit intent: fluency
Original:  It is based on the assumption that the layers are close to parallelHain , B.E., and Lomidze, M.G., 1995, Geotectonica s osnovami geodinamiki ( Geotectonics with basics of geodynamics):
Revised:  It is based on the assumption that the layers are close to parallel.Hain , B.E., and Lomidze, M.G., 1995, Geotectonica s osnovami geodinamiki ( Geotectonics with basics of geodynamics):
Edit intent: fluency
Original:  between key layer and target layerTearpock , Daniel J. and Bischke, Richard E. (2002), Applied Subsurface Geological Mapping with Structural Methods (2nd Edition), Prentice-Hall, Englewood Cliffs 822 p. . If the layers are parallel the distance between these layers is constant, the structures of both layers are identical, and to determine depths of the target horizon it is enough to get only one deep well, which reached the target layer.
Revised:  between key layer and target layer.Tearpock , Daniel J. and Bischke, Richard E. (2002), Applied Subsurface Geological Mapping with Structural Methods (2nd Edition), Prentice-Hall, Englewood Cliffs 822 p. . If the layers are parallel the distance between these layers is constant, the structures of both layers are identical, and to determine depths of the target horizon it is enough to get only one deep well, which reached the target layer.
Edit intent: fluency
Original:  between key layer and target layerTearpock , Daniel J. and Bischke, Richard E. (2002), Applied Subsurface Geological Mapping with Structural Methods (2nd Edition), Prentice-Hall, Englewood Cliffs 822 p. . If the layers are parallel the distance between these layers is constant, the structures of both layers are identical, and to determine depths of the target horizon it is enough to get only one deep well, which reached the target layer.
Revised:  between key layer and target layerTearpock , Daniel J. and Bischke, Richard E. (2002), Applied Subsurface Geological Mapping with Structural Methods (2nd Edition), Prentice-Hall, Englewood Cliffs 822 p. If the layers are parallel the distance between these layers is constant, the structures of both layers are identical, and to determine depths of the target horizon it is enough to get only one deep well, which reached the target layer.
Edit intent: fluency
Original:  In this case the standard procedure for calculating the distance between the target layer and key layer in any point in the area is linear interpolation between the known wellsYang Q. & Bursik M. A new interpolation method to model thickness, isopachs, extent, and volume of tephra fall deposits.
Revised:  In this case the standard procedure for calculating the distance between the target layer and key layer in any point in the area is linear interpolation between the known wells.Yang Q. & Bursik M. A new interpolation method to model thickness, isopachs, extent, and volume of tephra fall deposits.
Edit intent: fluency
Original:  Bulletin of Volcanology volume 78, article number 68 (2016) . . The reliability of the result (the geometrical structure of the target horizon) is estimated by the analysis of the trend of the distances between key horizon and target horizon (isopachs): if the trend is regular, for example, the distances are monotonically changing in one direction, it is a sign of reliability of the reconstruction.
Revised:  Bulletin of Volcanology volume 78, article number 68 (2016) . The reliability of the result (the geometrical structure of the target horizon) is estimated by the analysis of the trend of the distances between key horizon and target horizon (isopachs): if the trend is regular, for example, the distances are monotonically changing in one direction, it is a sign of reliability of the reconstruction.
Edit intent: fluency
Original:  born 4 January 1935 ) was a Malaysian barrister and judge who served as the second Chief Judge of Sabah and Sarawak.
Revised:  born 4 January 1934 ) was a Malaysian barrister and judge who served as the second Chief Judge of Sabah and Sarawak.
Edit intent: fluency
Original:  Category: 1935 births Category:
Revised:  Category: 1934 births Category:
Edit intent: style
Original:  born 4 January 1935  ) was a Malaysian barrister and judge who served as the second Chief Judge of Sabah and Sarawak.
Revised:  4 January 1935 ) was a Malaysian barrister and judge who served as the second Chief Judge of Sabah and Sarawak.
Edit intent: coherence
Original:  Chong's nephew and son of Chong Siew Chiang, Chong Chieng Jen, is the current Deputy Minister of Domestic Trade and Consumer Affairs of Malaysia  and Member of Parliament (MP) for Stampin.
Revised:  Chong's nephew and son of Chong Siew Chiang, Chong Chieng Jen, was previously the Deputy Minister of Domestic Trade and Consumer Affairs of Malaysia and Member of Parliament (MP) for Stampin.
Edit intent: style
Original:  Chairman of Matrix International Berhad (January 2003 to January 2006)
Edit intent: coherence
Original:  4 January 1935–23 January 2006) was a Malaysian barrister and judge who served as the second Chief Judge of Sabah and Sarawak.
Revised:  5 January 1935–23 January 2006) was a Malaysian barrister and judge who served as the second Chief Judge of Sabah and Sarawak.
Edit intent: fluency
Original:   4 January 1935 –23 January 2006 ) was a Malaysian barrister and judge who served as the second Chief Judge of Sabah and Sarawak.
Revised:  born 4 January 1935 –23 January 2006 ) was a Malaysian barrister and judge who served as the second Chief Judge of Sabah and Sarawak.
Edit intent: fluency
Original:   4 January 1935 –23 January 2006 ) was a Malaysian barrister and judge who served as the second Chief Judge of Sabah and Sarawak.
Revised:  4 January 1935 ) was a Malaysian barrister and judge who served as the second Chief Judge of Sabah and Sarawak.
Edit intent: coherence
Original:  Early life and education Chong was born in Sarikei in the then-British protectorate state of Raj of Sarawak to a emigrant Hakka couple who were owners of a Chinese drugstore.
Revised:  Early life and education Chong was born in Sarikei in the then-British protectorate state of Raj of Sarawak to a couple who were owners of a Chinese drugstore.
Edit intent: clarity
Original: Political career Manotoc ran as an provincial board member representing the 2nd Legislative district of Ilocos Norte in the 2016 Philippine local elections, and won.
Revised: Political career Manotoc ran as an provincial board member representing the 2nd legislative district of Ilocos Norte in the 2016 Philippine local elections, and won.
Edit intent: fluency
Original:  She was cast with ‘ clare-devil ’ Boman Shroff in a stream of successful stunt films  The Amazon, directed and produced by JBH Wadia, released on 1933.
Revised:  She was cast with ‘ dare-devil ’ Boman Shroff in a stream of successful stunt films The Amazon, directed and produced by JBH Wadia, released on 1933.
Edit intent: fluency
Original:  She was cast with ‘ clare-devil ’ Boman Shroff in a stream of successful stunt films  The Amazon, directed and produced by JBH Wadia, released on 1933.
Revised:  She was cast with ‘ clare-devil ’ Boman Shroff in a stream of successful stunt films such as The Amazon, directed and produced by JBH Wadia, released on 1933.
Edit intent: clarity
Original:  Padma Devi, Shrin Banu, M. Gupte, Badri Prasad, Gulab, Madhukar Gupte, Nandu Khote, Maruti Pahelwan, Raja Pandit, Ghulam Hussain, Master KamlakarBaburao PatelGandharva Cinetone1934MaharaniMubarak, Padma Devi, Shirin Banu, N. Chhapekar, Surve, Raja PanditBaburao PatelGandharva Cinetone1934Bhakta DhruvaMaster Muthu, T. Dwarkanath, H. S. Krishnamurthy Iyengar, T. Kanakalakshmamma,  Padma Devi, G. Nagesh, Devudu Narasimha Shastry, M. G. Mari RaoParshwanath AltekarU.
Revised:  Padma Devi, Shrin Banu, M. Gupte, Badri Prasad, Gulab, Madhukar Gupte, Nandu Khote, Maruti Pahelwan, Raja Pandit, Ghulam Hussain, Master KamlakarBaburao PatelGandharva Cinetone1934MaharaniMubarak, Padma Devi, Shirin Banu, N. Chhapekar, Surve, Raja PanditBaburao PatelGandharva Cinetone1934Bhakta DhruvaMaster Muthu, T. Dwarkanath, H. S. Krishnamurthy Iyengar, T. Kanakalakshmamma, S. K. Padma Devi, G. Nagesh, Devudu Narasimha Shastry, M. G. Mari RaoParshwanath AltekarU.
Edit intent: clarity
Original:  Sardar Akhtar, Padma Devi, Gope, Kamlakar, Omkar, Kamla Varekar, Sadiq Ali, Hari ShivdasaniRam DaryaniDaryani Production1937Kisan KanyaPadma Devi, Ghulam Mohammed , Sayed Ahmed, Jilloo Maa , Nissar, GaniMoti GidwaniArdeshir Irani of Imperial Pictures1937Do Auratein (Two Women)Padma Devi, Rose, Rafique Ghaznavi, Ghulam Mohammed, Baba Vyas, Sayed Ahmed, LaxmiMoti GidwaniImperial Pictures1938Kis LiyeMohini, Ghulam Mohammed, Padma Devi, Ghulam Rasool, Rafiqe Ghaznavi, AsujiJ.
Revised:  Sardar Akhtar, Padma Devi, Gope, Kamlakar, Omkar, Kamla Varekar, Sadiq Ali, Hari ShivdasaniRam DaryaniDaryani Production1937Kisan KanyaPadma Devi, Ghulam Md. , Sayed Ahmed, Jilloo Maa , Nissar, GaniMoti GidwaniArdeshir Irani of Imperial Pictures1937Do Auratein (Two Women)Padma Devi, Rose, Rafique Ghaznavi, Ghulam Mohammed, Baba Vyas, Sayed Ahmed, LaxmiMoti GidwaniImperial Pictures1938Kis LiyeMohini, Ghulam Mohammed, Padma Devi, Ghulam Rasool, Rafiqe Ghaznavi, AsujiJ.
Edit intent: coherence
Original:  Sardar Akhtar, Padma Devi, Gope, Kamlakar, Omkar, Kamla Varekar, Sadiq Ali, Hari ShivdasaniRam DaryaniDaryani Production1937Kisan KanyaPadma Devi, Ghulam Mohammed , Sayed Ahmed, Jilloo Maa , Nissar, GaniMoti GidwaniArdeshir Irani of Imperial Pictures1937Do Auratein (Two Women)Padma Devi, Rose, Rafique Ghaznavi, Ghulam Mohammed, Baba Vyas, Sayed Ahmed, LaxmiMoti GidwaniImperial Pictures1938Kis LiyeMohini, Ghulam Mohammed, Padma Devi, Ghulam Rasool, Rafiqe Ghaznavi, AsujiJ.
Revised:  Sardar Akhtar, Padma Devi, Gope, Kamlakar, Omkar, Kamla Varekar, Sadiq Ali, Hari ShivdasaniRam DaryaniDaryani Production1937Kisan KanyaPadma Devi, Ghulam Mohammed , Sayed Ahmed, Zilloo , Nissar, GaniMoti GidwaniArdeshir Irani of Imperial Pictures1937Do Auratein (Two Women)Padma Devi, Rose, Rafique Ghaznavi, Ghulam Mohammed, Baba Vyas, Sayed Ahmed, LaxmiMoti GidwaniImperial Pictures1938Kis LiyeMohini, Ghulam Mohammed, Padma Devi, Ghulam Rasool, Rafiqe Ghaznavi, AsujiJ.
Edit intent: clarity
Original:  R. SethiJaybharat Movies1938ZamanaNazir, Padma Devi, Hansa Wadkar, Jeevan, Majid , Vasant, Ameena, Bansi Karnataki, Gope, GulabRam DaryaniKrishna Movies1939Actress Kyon BaniUsha Rani, Ashiq Hussain, Padma Devi, Rafiqe Ghaznavi, W. M. Khan, Abdul, MukhtarG. R. SethiFederal Film Exchange1939Kaun Kisi KaShobhana Samarth, Khursheed, Padma Devi, Nazir, Mubarak, Gope, K. N. Singh, Maruti Rao, BibijanC.
Revised:  R. SethiJaybharat Movies1938ZamanaNazir, Padma Devi, Hansa Wadkar, Jeevan, Majeed , Vasant, Ameena, Bansi Karnataki, Gope, GulabRam DaryaniKrishna Movies1939Actress Kyon BaniUsha Rani, Ashiq Hussain, Padma Devi, Rafiqe Ghaznavi, W. M. Khan, Abdul, MukhtarG. R. SethiFederal Film Exchange1939Kaun Kisi KaShobhana Samarth, Khursheed, Padma Devi, Nazir, Mubarak, Gope, K. N. Singh, Maruti Rao, BibijanC.
Edit intent: fluency
Original:  R. SethiJaybharat Movies1938ZamanaNazir, Padma Devi, Hansa Wadkar, Jeevan, Majid , Vasant, Ameena, Bansi Karnataki, Gope, GulabRam DaryaniKrishna Movies1939Actress Kyon BaniUsha Rani, Ashiq Hussain, Padma Devi, Rafiqe Ghaznavi, W. M. Khan, Abdul, MukhtarG. R. SethiFederal Film Exchange1939Kaun Kisi KaShobhana Samarth, Khursheed, Padma Devi, Nazir, Mubarak, Gope, K. N. Singh, Maruti Rao, BibijanC.
Revised:  R. SethiJaybharat Movies1938ZamanaNazir, Padma Devi, Hansa Wadkar, Jeevan, Majid , Vasant, Ameena, Bansi Karnataki, Gope, Gulab, DarRam DaryaniKrishna Movies1939Actress Kyon BaniUsha Rani, Ashiq Hussain, Padma Devi, Rafiqe Ghaznavi, W. M. Khan, Abdul, MukhtarG. R. SethiFederal Film Exchange1939Kaun Kisi KaShobhana Samarth, Khursheed, Padma Devi, Nazir, Mubarak, Gope, K. N. Singh, Maruti Rao, BibijanC.
Edit intent: fluency
Original:  R. SethiJaybharat Movies1938ZamanaNazir, Padma Devi, Hansa Wadkar, Jeevan , Majeed, Vasant, Ameena, Bansi Karnataki, Gope, Gulab, DarRam DaryaniKrishna Movies1939Actress Kyon BaniUsha Rani, Ashiq Hussain, Padma Devi, Rafiqe Ghaznavi, W. M. Khan, Abdul, MukhtarG. R. SethiFederal Film Exchange1939Kaun Kisi KaShobhana Samarth, Khursheed, Padma Devi, Nazir, Mubarak, Gope, K. N. Singh, Maruti Rao, BibijanC.
Revised:  R. SethiJaybharat Movies1938ZamanaNazir, Padma Devi, Hansa Wadkar, Dar , Majeed, Vasant, Ameena, Bansi Karnataki, Gope, Gulab, DarRam DaryaniKrishna Movies1939Actress Kyon BaniUsha Rani, Ashiq Hussain, Padma Devi, Rafiqe Ghaznavi, W. M. Khan, Abdul, MukhtarG. R. SethiFederal Film Exchange1939Kaun Kisi KaShobhana Samarth, Khursheed, Padma Devi, Nazir, Mubarak, Gope, K. N. Singh, Maruti Rao, BibijanC.
Edit intent: clarity