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Experimental results also show that the fractionation of the carbon isotope of methane of coal core desorption gas changes very little; the δ\u003Cjats:sup>13\u003C\u002Fjats:sup>C\u003Cjats:sub>1\u003C\u002Fjats:sub> value of the mixed gas of biogenic and thermogenic gases is between the δ\u003Cjats:sup>13\u003C\u002Fjats:sup>C\u003Cjats:sub>1\u003C\u002Fjats:sub> values of the two “original” gases, and the value is determined by the carbon isotopic compositions and mixing proportions of the two “original” methanes. Therefore this paper proposes that the study on the secondary changes of the thermogenic gas and various additive effects is a new effective way to study and identify SBG. Herein, a systematic example of research on the coalbed gas (Huainan coalbed gas) is further conducted, revealing a series of secondary changes and additive effects, the main characteristics and markers of which are: (1) the contents of CO\u003Cjats:sub>2\u003C\u002Fjats:sub> and heavy‐hydrocarbons decrease significantly; (2) the content of CH\u003Cjats:sub>4\u003C\u002Fjats:sub> increases and the gas becomes drier; (3) the δ\u003Cjats:sup>13\u003C\u002Fjats:sup>C and δD values of methane decrease significantly and tend to have biogenetic characteristics; and (4) the values of δ\u003Cjats:sup>13\u003C\u002Fjats:sup>C\u003Cjats:sub>2\u003C\u002Fjats:sub> and δ\u003Cjats:sup>13\u003C\u002Fjats:sup>C\u003Cjats:sc>co\u003C\u002Fjats:sc>\u003Cjats:sub>2\u003C\u002Fjats:sub> grow higher. These isotopic values also change with the degradation degrees by microbes and mixing proportions of the two kinds of gases in different locations. There exists a negative correlation between the δ\u003Cjats:sup>13\u003C\u002Fjats:sup>C\u003Cjats:sub>1\u003C\u002Fjats:sub>\u003Cjats:italic>vs\u003C\u002Fjats:italic>δ\u003Cjats:sup>13\u003C\u002Fjats:sup>C\u003Cjats:sc>co\u003C\u002Fjats:sc>\u003Cjats:sub>2\u003C\u002Fjats:sub> values. The Δδ\u003Cjats:sup>13\u003C\u002Fjats:sup>C\u003Cjats:sc>c\u003C\u002Fjats:sc>\u003Cjats:sub>2\u003C\u002Fjats:sub>–\u003Cjats:sc>c\u003C\u002Fjats:sc>\u003Cjats:sub>1\u003C\u002Fjats:sub> values obviously become higher. The distributions of the Δδ\u003Cjats:sup>13\u003C\u002Fjats:sup>C\u003Cjats:sc>co\u003C\u002Fjats:sc>\u003Cjats:sub>2\u003C\u002Fjats:sub>–\u003Cjats:sc>c\u003C\u002Fjats:sc>\u003Cjats:sub>1\u003C\u002Fjats:sub> values are within certain limits and show regularity. There exist a positive correlation between the N\u003Cjats:sub>2\u003C\u002Fjats:sub> versus Ar contents, and a negative correlation between the N\u003Cjats:sub>2\u003C\u002Fjats:sub> versus CH\u003Cjats:sub>4\u003C\u002Fjats:sub> contents, indicating the down forward infiltration of the surface water containing air. These are important markers of the generation and existence of SBG.\u003C\u002Fjats:p>",{"EN":909},"New Approaches and Markers for Identifying Secondary Biogenic Coalbed Gas",{"VOID":911},"10.1111\u002Fj.1755-6724.2012.00622.x",[107],"https:\u002F\u002Fonlinelibrary.wiley.com\u002Fdoi\u002F10.1111\u002Fj.1755-6724.2012.00622.x",[915,934,949,974,989,1006,1023,1038,1053],{"id":916,"sortIndex":25,"researcher":24,"roles":917,"affiliations":918,"properties":927,"displayName":931,"givenName":24,"familyName":24},"7fa42e2f-9efa-4ab0-b0fa-e5f6e7e4b745",[],[919],{"id":920,"sortIndex":25,"affiliation":921,"properties":24},"c38d1e44-2d84-4fe6-aa0f-8ee2b66904a4",{"id":920,"createTime":24,"updateTime":24,"relativeEntities":922,"slug":24,"properties":923,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":926,"statistic":24},[],{"title":924},{"EN":925},"College of Resource Science and Technology\u002F Key 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development of the weathering crust of the granite intrusions in the Longnan area, Jiangxi Province. REE is mostly concentrated in an adsorption state in clay in the wholly weathered zone. The rare‐earth minerals enriched in the parent rocks provided the source material for the REE enrichment. Exchangeable REE accounts for 48‐86%. Extraction experiments and stable isotopic study of clay minerals suggest that the downward infiltration of meteoric water and increasing gradient of pH values have played an important role in the enrichment of REE during the progressive weathering. 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Andaman Forearc Basin (AFB) is asymmetric in configuration and filled with a ∼6 km‐thick pile of Neogene to Recent sediments (∼4 s in two‐way travel time: TWT) with distinct zonation. It shows gradual thinning up to ∼3 km (0.8 s in TWT) towards the eastern end with a seabed gradient of 1:30. Thick deformed sediments ∼2 s (TWT) of the Outerarc are associated with intense faulting and occasional folding caused by recent tectonics. Development of a series of faults within the upwarped sedimentary column of Oligocene top to Recent is observed with a rotated fault block. These features are manifestations of Recent igneous intrusion, and reveal the presence of a mild N–S compressional regime. Its effect on the AFB resulted in further uplift of sediments, which can now be seen as the Invisible Bank. Forward gravity modelling supporting our seismic interpretation reveals that it is associated with igneous intrusion from the Moho (∼9 km depth), and also suggests that continental crust underlies the AFB. Strong Bottom Simulating Reflector (BSR)‐like features in the Miocene sediments of Outerarc and Forearc basin at a depth of 0.6 s below the seabed suggest the inferred probable occurrence of gas hydrates in the AFB.\u003C\u002Fjats:p>",{"EN":1620},"Structural Characteristics of the Andaman Forearc Inferred from Interpretation of Multichannel Seismic Reflection Data",{"VOID":1622},"10.1111\u002F1755-6724.12279",[107],"https:\u002F\u002Fonlinelibrary.wiley.com\u002Fdoi\u002F10.1111\u002F1755-6724.12279",[1626,1643],{"id":1627,"sortIndex":25,"researcher":24,"roles":1628,"affiliations":1629,"properties":1638,"displayName":1640,"givenName":24,"familyName":24},"1723fe37-aa31-47b3-b257-e7a5c654b179",[],[1630],{"id":1631,"sortIndex":25,"affiliation":1632,"properties":24},"0e864be0-6243-45e2-a727-d035bd156368",{"id":1631,"createTime":24,"updateTime":24,"relativeEntities":1633,"slug":24,"properties":1634,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":1637,"statistic":24},[],{"title":1635},{"EN":1636},"National Centre for Antarctic and Ocean Research Vasco da Gama Goa‐403 804 India",[],{"title":1639,"openalex":1641},{"EN":1640},"Goli Anitha",{"VOID":1642},"A5067719412",{"id":1644,"sortIndex":124,"researcher":24,"roles":1645,"affiliations":1646,"properties":1653,"displayName":1657,"givenName":24,"familyName":24},"5cbf87b8-3adc-49da-8896-6390e938139d",[],[1647],{"id":1631,"sortIndex":25,"affiliation":1648,"properties":24},{"id":1631,"createTime":24,"updateTime":24,"relativeEntities":1649,"slug":24,"properties":1650,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":1652,"statistic":24},[],{"title":1651},{"EN":1636},[],{"orcid":1654,"title":1656,"openalex":1658},{"VOID":1655},"https:\u002F\u002Forcid.org\u002F0000-0001-6899-8995",{"EN":1657},"Dhananjai K. Pandey",{"VOID":1659},"A5091744561",{"url":24,"publisher":1661,"properties":1699},{"id":6,"createTime":7,"updateTime":8,"relativeEntities":1662,"slug":10,"properties":1663,"entityType":22,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":25,"subjectFields":1668,"manageAffiliations":1673,"indexDatabases":1684,"url":83,"thumbnailPath":24,"statistic":24,"gsStatistic":24,"type":24,"analyzePriority":24},[],{"country":1664,"eissn":1665,"issn":1666,"title":1667},{"VOID":13},{"VOID":15},{"VOID":17},{"EN":19},[1669],{"id":28,"createTime":24,"updateTime":24,"relativeEntities":1670,"label":1671,"description":1672,"parentId":24,"standard":24,"scholarHubFieldId":24},[],{"EN":31},{},[1674,1679],{"id":35,"createTime":24,"updateTime":24,"relativeEntities":1675,"slug":24,"properties":1676,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":1678,"statistic":24},[],{"title":1677},{"EN":39},[],{"id":42,"createTime":24,"updateTime":24,"relativeEntities":1680,"slug":24,"properties":1681,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":1683,"statistic":24},[],{"title":1682},{"EN":46},[],[1685,1692],{"id":50,"indexDatabase":1686,"url":63,"indexYears":24,"academicFieldIds":1691,"indexDatabaseRanking":24},{"id":52,"createTime":24,"updateTime":24,"relativeEntities":1687,"label":1688,"description":1689,"key":59,"publicationTags":1690,"standard":24},[],{"EN":55,"VI":55},{"EN":57,"VI":58},[61,62],[65],{"id":67,"indexDatabase":1693,"url":78,"indexYears":79,"academicFieldIds":1698,"indexDatabaseRanking":82},{"id":69,"createTime":24,"updateTime":24,"relativeEntities":1694,"label":1695,"description":1696,"key":75,"publicationTags":1697,"standard":24},[],{"EN":72,"VI":72},{"EN":72,"VI":74},[77],[81],{"issue":1700,"pages":1702,"volume":1704},{"VOID":1701},"4",{"VOID":1703},"1145-1156",{"VOID":1705},"88",14,{"total":1706,"publishYear":1708,"statisticByYear":1709},2014,{"2015":133,"2016":124,"2017":512,"2018":133,"2020":133,"2023":124},"2014-08-01",[82,61],[1713,1716,1719,1722,1725,1728,1731,1734,1737,1740,1743,1746,1749,1752,1755,1758,1761,1764,1767,1770,1773,1776,1779,1782,1785,1788],{"id":24,"text":1714,"url":24,"identifiers":1715},"Bull J.M., 1990, Structural style of Intra-plate deformation, central Indian Ocean Basin: Evidence for the role of fracture zones, Tectonophysics, 25, 213228",{},{"id":24,"text":1717,"url":24,"identifiers":1718},"Collett T.S., 2008, Directorate General of Hydrocarbons",{},{"id":24,"text":1720,"url":24,"identifiers":1721},"10.1016\u002Fj.jseaes.2004.09.001",{"doi":1720},{"id":24,"text":1723,"url":24,"identifiers":1724},"Curray J.R., 1979, Tectonics of the Andaman Sea and Burma, American Association of Petroleum Geolology. Memoir, 29, 189",{},{"id":24,"text":1726,"url":24,"identifiers":1727},"10.1007\u002F978-1-4615-8038-6_9",{"doi":1726},{"id":24,"text":1729,"url":24,"identifiers":1730},"10.1016\u002F0040-1951(93)90314-A",{"doi":1729},{"id":24,"text":1732,"url":24,"identifiers":1733},"10.1023\u002FA:1023520105384",{"doi":1732},{"id":24,"text":1735,"url":24,"identifiers":1736},"10.1016\u002FS0264-3707(03)00062-0",{"doi":1735},{"id":24,"text":1738,"url":24,"identifiers":1739},"Hamilton W., 1979, Geological Survey Professional Paper 1078: 1 plate",{},{"id":24,"text":1741,"url":24,"identifiers":1742},"10.1130\u002F0016-7606(1988)100\u003C1503:PTAIA>2.3.CO;2",{"doi":1741},{"id":24,"text":1744,"url":24,"identifiers":1745},"10.1029\u002F2000JB000095",{"doi":1744},{"id":24,"text":1747,"url":24,"identifiers":1748},"10.1029\u002F2002TC001420",{"doi":1747},{"id":24,"text":1750,"url":24,"identifiers":1751},"Zhonghai Li, 2013, Dynamics of India-Asia Collision from 2-D and 3-D numerical modeling, Acta Geologica Sinica (English Edition), 87, 142",{},{"id":24,"text":1753,"url":24,"identifiers":1754},"10.1016\u002Fj.tecto.2010.06.008",{"doi":1753},{"id":24,"text":1756,"url":24,"identifiers":1757},"10.1306\u002F111302730367",{"doi":1756},{"id":24,"text":1759,"url":24,"identifiers":1760},"10.1016\u002Fj.tecto.2008.08.021",{"doi":1759},{"id":24,"text":1762,"url":24,"identifiers":1763},"10.1016\u002FS0012-821X(04)00075-5",{"doi":1762},{"id":24,"text":1765,"url":24,"identifiers":1766},"10.1029\u002F2006GL028730",{"doi":1765},{"id":24,"text":1768,"url":24,"identifiers":1769},"10.1029\u002F1999GL005396",{"doi":1768},{"id":24,"text":1771,"url":24,"identifiers":1772},"10.1130\u002F0016-7606(1969)80[1203:BAMGOT]2.0.CO;2",{"doi":1771},{"id":24,"text":1774,"url":24,"identifiers":1775},"Roy T.K., 1987, Wrench faulting in Andaman Forearc basin, India, Proceedings of the Offshore Technology Conference, 19, 393",{},{"id":24,"text":1777,"url":24,"identifiers":1778},"10.1029\u002F2000JB900120",{"doi":1777},{"id":24,"text":1780,"url":24,"identifiers":1781},"10.1029\u002F2005EO480002",{"doi":1780},{"id":24,"text":1783,"url":24,"identifiers":1784},"10.1126\u002Fscience.277.5334.1956",{"doi":1783},{"id":24,"text":1786,"url":24,"identifiers":1787},"10.1016\u002Fj.epsl.2007.10.016",{"doi":1786},{"id":24,"text":1789,"url":24,"identifiers":1790},"10.1016\u002FS0743-9547(96)00068-2",{"doi":1789},{"id":1792,"createTime":1793,"updateTime":1793,"relativeEntities":1794,"slug":1795,"properties":1796,"entityType":102,"verifyStatus":103,"verifyTime":1793,"verifyNote":105,"languages":1807,"translateLanguages":24,"viewCount":25,"primaryUrl":1808,"fullTextUrl":24,"authors":1809,"publicationType":147,"publisherRelationship":1848,"citationCount":1893,"citationInfo":1894,"publishDate":1897,"publishYear":1895,"citationAnalyzeStatus":23,"lastCitationAnalyze":24,"indexDatabases":1898,"openAccess":24,"references":1899,"isForceReanalyzing":245},"8b979163-7ff4-446c-a193-679adcfdc51f","2024-10-11T09:20:18.599+00:00",[],"Lower-Triassic-and-Induan-Olenekian-Boundary-in-Chaohu-Anhui-Province-South-China",{"openalex":1797,"mag":1799,"abstract":1801,"title":1803,"doi":1805},{"VOID":1798},"W2063823610",{"VOID":1800},"2063823610",{"EN":1802},"\u003Cjats:title>Abstract:\u003C\u002Fjats:title>\u003Cjats:p>Since the West Pingdingshan Section in Chaohu was proposed as the candidate of the Global Stratotype Section and Point of the Induan‐Olenekian boundary in 2003, the Lower Triassic of Chaohu has been extensively studied. Based on the studies on the Lower Triassic of Chaohu, (1) a continuous conodont zonation is established, which has become an important reference for Lower Triassic stratigraphic correlation over the world; (2) the First Appearance Datum of conodont \u003Cjats:italic>Neospathodus waageni\u003C\u002Fjats:italic> was suggested and has been basically accepted as the primary marker to define the Induan‐Olenekian boundary; (3) a characteristic Lower Triassic excursion of carbon isotopes was brought to light and has been proven to be not only an excellent index for the stratigraphic correlation but also a unique indication for the perturbation of ecological environments in the aftermath of the end‐Permian mass extinction; (4) a magnetostratigraphic sequence is constituted with a certain biostratigraphic control in the low‐latitude region and it presents an important correlation to the Boreal sequence; (5) a cyclostratigraphic study provides an alternative method to constrain the age of the chronostratigraphic units; and (6) a scheme of the Olenekian subdivision is recently suggested to define the boundary between the Smithian and Spathian Substages. In addition, Chaohu is also the type locality of the Chaohuan Stage, the upper stage of the Lower Triassic in the China Chronostratigraphic System. Thus, the Lower Triassic of Chaohu is not only a classic sequence in South China, but also a key reference sequence to the investigation of the corresponding stratigraphy and geological events over the world. The recent achievements are viewed here for an overall understanding of the sequence. Then the current situation of the Induan‐Olenekian and Smithian‐Spathian boundaries is discussed to provide a reference for later works.\u003C\u002Fjats:p>",{"EN":1804},"Lower Triassic and Induan‐Olenekian Boundary in Chaohu, Anhui Province, South China",{"VOID":1806},"10.1111\u002Fj.1755-6724.2011.00408.x",[107],"https:\u002F\u002Fonlinelibrary.wiley.com\u002Fdoi\u002F10.1111\u002Fj.1755-6724.2011.00408.x",[1810,1829],{"id":1811,"sortIndex":25,"researcher":24,"roles":1812,"affiliations":1813,"properties":1822,"displayName":1826,"givenName":24,"familyName":24},"20b073ca-4015-4b09-a9cd-6786b37698ef",[],[1814],{"id":1815,"sortIndex":25,"affiliation":1816,"properties":24},"2d7226cf-3594-428d-99b1-65e1cdb0fd50",{"id":1815,"createTime":24,"updateTime":24,"relativeEntities":1817,"slug":24,"properties":1818,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":1821,"statistic":24},[],{"title":1819},{"VI":1820},"Key Laboratory of Biogeology and Environmental Geology of Ministry of Education, China University of Geosciences, Wuhan 430074, China",[],{"orcid":1823,"title":1825,"openalex":1827},{"VOID":1824},"https:\u002F\u002Forcid.org\u002F0000-0002-3142-8312",{"EN":1826},"Jinnan Tong",{"VOID":1828},"A5010964979",{"id":1830,"sortIndex":124,"researcher":24,"roles":1831,"affiliations":1832,"properties":1841,"displayName":1845,"givenName":24,"familyName":24},"502c1eb3-3728-48f2-beb1-0bb41997dffa",[],[1833],{"id":1834,"sortIndex":25,"affiliation":1835,"properties":24},"18307257-7595-40be-b8ab-1ea840a0fa94",{"id":1834,"createTime":24,"updateTime":24,"relativeEntities":1836,"slug":24,"properties":1837,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":1840,"statistic":24},[],{"title":1838},{"VI":1839},"State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China",[],{"orcid":1842,"title":1844,"openalex":1846},{"VOID":1843},"https:\u002F\u002Forcid.org\u002F0000-0001-9914-0385",{"EN":1845},"Laishi Zhao",{"VOID":1847},"A5010921521",{"url":24,"publisher":1849,"properties":1887},{"id":6,"createTime":7,"updateTime":8,"relativeEntities":1850,"slug":10,"properties":1851,"entityType":22,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":25,"subjectFields":1856,"manageAffiliations":1861,"indexDatabases":1872,"url":83,"thumbnailPath":24,"statistic":24,"gsStatistic":24,"type":24,"analyzePriority":24},[],{"country":1852,"eissn":1853,"issn":1854,"title":1855},{"VOID":13},{"VOID":15},{"VOID":17},{"EN":19},[1857],{"id":28,"createTime":24,"updateTime":24,"relativeEntities":1858,"label":1859,"description":1860,"parentId":24,"standard":24,"scholarHubFieldId":24},[],{"EN":31},{},[1862,1867],{"id":35,"createTime":24,"updateTime":24,"relativeEntities":1863,"slug":24,"properties":1864,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":1866,"statistic":24},[],{"title":1865},{"EN":39},[],{"id":42,"createTime":24,"updateTime":24,"relativeEntities":1868,"slug":24,"properties":1869,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":1871,"statistic":24},[],{"title":1870},{"EN":46},[],[1873,1880],{"id":50,"indexDatabase":1874,"url":63,"indexYears":24,"academicFieldIds":1879,"indexDatabaseRanking":24},{"id":52,"createTime":24,"updateTime":24,"relativeEntities":1875,"label":1876,"description":1877,"key":59,"publicationTags":1878,"standard":24},[],{"EN":55,"VI":55},{"EN":57,"VI":58},[61,62],[65],{"id":67,"indexDatabase":1881,"url":78,"indexYears":79,"academicFieldIds":1886,"indexDatabaseRanking":82},{"id":69,"createTime":24,"updateTime":24,"relativeEntities":1882,"label":1883,"description":1884,"key":75,"publicationTags":1885,"standard":24},[],{"EN":72,"VI":72},{"EN":72,"VI":74},[77],[81],{"issue":1888,"pages":1889,"volume":1891},{"VOID":1304},{"VOID":1890},"399-407",{"VOID":1892},"85",29,{"total":1893,"publishYear":1895,"statisticByYear":1896},2011,{"2012":462,"2013":462,"2014":462,"2015":124,"2016":480,"2017":124,"2018":480,"2019":133,"2020":124,"2021":124,"2022":133,"2023":462},"2011-04-01",[82,61],[1900,1903,1906,1909,1912,1915,1918,1921,1924,1927,1930,1933,1936,1939,1942,1945,1948,1951,1954,1957,1961,1964,1967,1970,1973,1976,1979,1982,1985,1988,1991,1994,1997,2000,2003,2006,2009,2012,2015,2018,2021,2024,2028,2031,2034,2037,2040,2043,2046,2049,2052],{"id":24,"text":1901,"url":24,"identifiers":1902},"10.1016\u002Fj.palaeo.2006.02.003",{"doi":1901},{"id":24,"text":1904,"url":24,"identifiers":1905},"Yanyue Cao, 1993, Conodonts of Lower Yangtze Valley—An Indexes to Biostratigraphy and Organic Metamorphic Maturity, 114",{},{"id":24,"text":1907,"url":24,"identifiers":1908},"China National Stratigraphic Commission, 2002, A Manual for the Regional Chronostratigraphic (Chronologic) Table of China",{},{"id":24,"text":1910,"url":24,"identifiers":1911},"DingMeihua 1983.Lower Triassic conodonts from Mount Majiashan in Anhui Province and their stratigraphic significance.Earth Science—Journal of China University of Geosciences (2):37–48(in Chinese with English abstract).",{},{"id":24,"text":1913,"url":24,"identifiers":1914},"Zengzhao Feng, Study on Lithofacies Paleogeography of Qinglong Group of Lower‐Middle Triassic in the Lower Yangtze River Region",{},{"id":24,"text":1916,"url":24,"identifiers":1917},"10.1130\u002FG23117A.1",{"doi":1916},{"id":24,"text":1919,"url":24,"identifiers":1920},"10.1016\u002Fj.epsl.2007.04.023",{"doi":1919},{"id":24,"text":1922,"url":24,"identifiers":1923},"10.1016\u002Fj.palaeo.2006.08.014",{"doi":1922},{"id":24,"text":1925,"url":24,"identifiers":1926},"10.1007\u002Fs11430-007-0156-z",{"doi":1925},{"id":24,"text":1928,"url":24,"identifiers":1929},"Peixia Guo, 1982, On the occurrence of late Lower Triassic ammonoids from Anhui and Jiangsu, Acta Palaeontologica Sinica, 21, 560",{},{"id":24,"text":1931,"url":24,"identifiers":1932},"Peixia Guo, 1980, Knowledge on the age of Qinglong Group in Chaoxian, Anhui Province, Journal of Stratigraphy, 4, 310",{},{"id":24,"text":1934,"url":24,"identifiers":1935},"10.1016\u002Fj.palaeo.2006.11.049",{"doi":1934},{"id":24,"text":1937,"url":24,"identifiers":1938},"10.1016\u002Fj.palaeo.2006.11.052",{"doi":1937},{"id":24,"text":1940,"url":24,"identifiers":1941},"Korte C., 2007, Carbon isotope values of Triassic lacustrine and hypersaline playa‐lake carbonates: Lower Buntsandstein and Middle Keuper (Germany), Hallesches Jahrb. Geowiss., 29, 1",{},{"id":24,"text":1943,"url":24,"identifiers":1944},"Krystyn L., 2007, A candidate GSSP for the base of the Olenekian Stage: Mud at Pin Valley; district Lahul & Spiti, Himachal Pradesh (Western Himalaya), India, Albertiana, 35, 5",{},{"id":24,"text":1946,"url":24,"identifiers":1947},"10.1016\u002Fj.palaeo.2006.11.043",{"doi":1946},{"id":24,"text":1949,"url":24,"identifiers":1950},"Dan Liang, 2011, Lower Triassic Smithian‐Spathian boundary at West Pingdingshan Section in Chaohu, Anhui Province, Science China: Earth Science, 41, 149",{},{"id":24,"text":1952,"url":24,"identifiers":1953},"10.1126\u002Fscience.1101012",{"doi":1952},{"id":24,"text":1955,"url":24,"identifiers":1956},"10.1016\u002Fj.palaeo.2006.11.037",{"doi":1955},{"id":24,"text":1958,"url":24,"identifiers":1959},"Yuanqiao Peng, 2001, The Permian‐Triassic boundary set: characteristics and correlation, Newsletters on Stratigraphy, 39, 55, 10.1127\u002Fnos\u002F39\u002F2001\u002F55",{"doi":1960},"10.1127\u002Fnos\u002F39\u002F2001\u002F55",{"id":24,"text":1962,"url":24,"identifiers":1963},"10.1016\u002FS0031-0182(03)00310-9",{"doi":1962},{"id":24,"text":1965,"url":24,"identifiers":1966},"Salvador A., 1994, International Stratigraphic Guide, 214",{},{"id":24,"text":1968,"url":24,"identifiers":1969},"10.1002\u002Fgj.1232",{"doi":1968},{"id":24,"text":1971,"url":24,"identifiers":1972},"10.1016\u002Fj.epsl.2009.01.009",{"doi":1971},{"id":24,"text":1974,"url":24,"identifiers":1975},"10.1016\u002Fj.epsl.2007.07.018",{"doi":1974},{"id":24,"text":1977,"url":24,"identifiers":1978},"Jinnan Tong, 2002, Lower Triassic inorganic carbon isotope excursion in Chaohu, Anhui Province, China, Journal of China University of Geosciences, 13, 98",{},{"id":24,"text":1980,"url":24,"identifiers":1981},"10.1007\u002FBF02973113",{"doi":1980},{"id":24,"text":1983,"url":24,"identifiers":1984},"10.1016\u002FS1367-9120(01)00058-X",{"doi":1983},{"id":24,"text":1986,"url":24,"identifiers":1987},"Jinnan Tong, 2009, Advance in the study of Early Triassic life and environment, Acta Palaeontologica Sinica, 48, 497",{},{"id":24,"text":1989,"url":24,"identifiers":1990},"10.1007\u002FBF02875389",{"doi":1989},{"id":24,"text":1992,"url":24,"identifiers":1993},"Jinnan Tong, 2004, Lower Triassic Ammonoid Zonation in Chaohu, Anhui Province, China, Albertiana, 31, 65",{},{"id":24,"text":1995,"url":24,"identifiers":1996},"10.1360\u002F03yd0295",{"doi":1995},{"id":24,"text":1998,"url":24,"identifiers":1999},"Jinnan Tong, 2004, Early Triassic ammonoid succession in Chaohu, Anhui Province, Acta Palaeontologica Sinica, 43, 192",{},{"id":24,"text":2001,"url":24,"identifiers":2002},"Jinnan Tong, 2002, Report on the field excursion to Chaohu, Anhui Province, South China, Albertiana, 27, 26",{},{"id":24,"text":2004,"url":24,"identifiers":2005},"Jinnan Tong, 2005, An integrated Lower Triassic sequence in Chaohu, Anhui Province, Earth Science—Journal of China University of Geosciences, 30, 40",{},{"id":24,"text":2007,"url":24,"identifiers":2008},"10.1666\u002F0022-3360(2006)080[0146:FFFTLT]2.0.CO;2",{"doi":2007},{"id":24,"text":2010,"url":24,"identifiers":2011},"10.1002\u002Fgj.1084",{"doi":2010},{"id":24,"text":2013,"url":24,"identifiers":2014},"Tozer E.T., 1965, Lower Triassic stages and ammonoid zones of Arctic Canada, Geological Survey of Canada Paper, 65, 1",{},{"id":24,"text":2016,"url":24,"identifiers":2017},"10.1080\u002F00241160410006500",{"doi":2016},{"id":24,"text":2019,"url":24,"identifiers":2020},"Zunyi Yang, Permian‐Triassic Boundary Stratigraphy and Fauna of South China",{},{"id":24,"text":2022,"url":24,"identifiers":2023},"Hongfu Yin, 1999, South China defined as part of Tethyan Archipelagic Ocean, Earth Science—Journal of China University of Geosciences, 24, 1",{},{"id":24,"text":2025,"url":24,"identifiers":2026},"Hongfu Yin, 2001, The Global Stratotype Section and Point (GSSP) of the Permian‐Triassic boundary, Episodes, 24, 102, 10.18814\u002Fepiiugs\u002F2001\u002Fv24i2\u002F004",{"doi":2027},"10.18814\u002Fepiiugs\u002F2001\u002Fv24i2\u002F004",{"id":24,"text":2029,"url":24,"identifiers":2030},"Zakharov Y.D., 1994, Stratotype of the Induan‐Olenekian boundary of the Lower Triassic, Tikhookeanskaya Geologiya, 1994, 33",{},{"id":24,"text":2032,"url":24,"identifiers":2033},"Zakharov Y.D., 1996, The Induan‐Olenekian boundary in the Tethys and Boreal realms. Ann. Mus. Civ. Rovereto., Sec. Arch., Sc. Nat., Suppl. 11 (1995): 133–156. Zakharov, Y.D., 2010. New information on biostratigraphy of the Mud section, Spiti, Himalayas, Albertiana, 38, 4",{},{"id":24,"text":2035,"url":24,"identifiers":2036},"Zakharov Y.D., 2000, The candidates of global stratotype of the boundary of the Induan and Olenekian stages of the Lower Triassic in southern Primorye, Albertiana, 24, 14",{},{"id":24,"text":2038,"url":24,"identifiers":2039},"Zakharov Y.D., 2002, Candidates for global stratotype of the Induan‐Olenekian boundary in South Primorye, Strat. Geol. 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The boundary ages for MGS1 (the Dishaogouwan and Dagouwan Formations), MGS2 (the upper Chengchuan Formation), MGS3 (the middle Chengchuan Formation), MGS4 (the lower Chengchuan Formation), MGS5 (most strata of the Salawusu Formation) and MGS6 (the bottom of the Salawusu Formation and the top of the Lishi Formation) correspond to those of MIS1, MIS2, MIS3, MIS4, MIS5 and MIS6, respectively, from deep sea sediments or continental glaciers. MGS5 can be subdivided into five subsegments (MGS5a, MGS5b, MGS5c, MGS5d and MGS5e) and the boundary ages of these subsegments correspond to those of MIS5a, MIS5b, MIS5c, MIS5d and MIS5e, respectively. Based on the paleoenvironment and paleoecology indicated by the primary chemical elements, fossil vertebrates, mollusks and pollen grains, we hypothesize that MGS1, MGS2, MGS3, MGS4, MGS5 and MGS6 and the subsegments of MGS5 match the corresponding stages for oxygen isotopes in the deep sea sediments and continental glaciers, and the substages of MIS5 in terms of climatic characters, further explaining the phenomena that determined the formation of the late Quaternary strata and the paleontology of the Salawusu River valley. These phenomena relate to fluctuations in the global climate (and particularly in the East Asian monsoon) during the glacial and interglacial periods.\u003C\u002Fjats:p>",{"EN":2068},"Phases of Environmental Evolution Indicated by Primary Chemical Elements and Paleontological Records in the Upper Pleistocene‐Holocene Series for the Salawusu River Valley, 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Sinica, 2, 90",{},{"id":24,"text":2429,"url":24,"identifiers":2430},"Yühong Zhang, 2001, Grain‐size cycles in Salawusu River Valley since 150,000a BP, Acta Geographica Sinica, 11, 461",{},{"id":24,"text":2432,"url":24,"identifiers":2433},"Honghan Zheng, 1989, Late Pleistocene fluvio‐lacustrine deposits and eolian loess in North China, Geochimica, 4, 343",{},{"id":24,"text":2435,"url":24,"identifiers":2436},"Kunshu Zhou, 1982, Contribution to the Academic Symposium on the Pre‐Historic Earthquake and Geology of China, 149",{},{"id":24,"text":2438,"url":24,"identifiers":2439},"Kunshu Zhou, 1987, Habitation environment of the Fossil Ordos Man and the geological age, 97",{},{"id":2441,"createTime":2442,"updateTime":2442,"relativeEntities":2443,"slug":2444,"properties":2445,"entityType":102,"verifyStatus":103,"verifyTime":2456,"verifyNote":105,"languages":2457,"translateLanguages":24,"viewCount":25,"primaryUrl":2458,"fullTextUrl":24,"authors":2459,"publicationType":147,"publisherRelationship":2562,"citationCount":2606,"citationInfo":2607,"publishDate":2609,"publishYear":1708,"citationAnalyzeStatus":23,"lastCitationAnalyze":24,"indexDatabases":2610,"openAccess":24,"references":2611,"isForceReanalyzing":245},"6a5b9438-6ee3-4c4d-899b-1997a922e89d","2024-10-05T15:02:56.259+00:00",[],"Prospects-of-Carboniferous-Shale-Gas-Exploitation-in-the-Eastern-Qaidam-Basin",{"openalex":2446,"mag":2448,"abstract":2450,"title":2452,"doi":2454},{"VOID":2447},"W2161332843",{"VOID":2449},"2161332843",{"EN":2451},"\u003Cjats:title>Abstract:\u003C\u002Fjats:title>\u003Cjats:p>Shale gas is a resource of emerging importance in the energy field. Many countries in the world have been making big financial investments in this area. Carboniferous shale in the eastern Qaidam Basin shows good exploration prospects, but limited research and exploration work for shale oil and gas resources has been undertaken. Geochemical analyses were performed on shale derived from the Upper Carboniferous Hurleg Formation in the eastern Qaidam Basin, Qinghai Province, and secondary electron imaging capability of a Field Emission scanning electron microscope (FE‐SEM) was used to characterize the microstructure of the shale. The reservoir and exploitation potential of the studied shale was assessed by comparison with research results obtained from the Barnett Formation shale in Fort Worth Basin, North America and the Basin shale of Sichuan province. The results indicate that the eastern Qaidam Basin Carboniferous shale is high‐quality source rock. There are four major microstructural types in the study area: matrix intergranular pores, dissolution pores, intergranular pores, and micro‐fractures. The size of the micropores varies from 6–633 nm, the majority of which is between 39–200 nm, with a relatively small number of micro‐scale pores ranging from 0.13–1 μm. The pore characteristics of the studied shales are similar to the North American and Sichuanese shales, indicating that they have good reservoir potential. No micropores are present in the organic matter, which is induced by its composition; instead we found an important lamellar structure in the organic matter. These micropores and microfractures are abundant, and are connected to natural visible cracks that form the network pore system, which controls the storage and migration of shale gas. This connectivity is favorable for shale gas exploitation, providing great scientific potential and practical value.\u003C\u002Fjats:p>",{"EN":2453},"Prospects of Carboniferous Shale Gas Exploitation in the Eastern Qaidam 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Ambrose R.J. 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Ray J. andCarl H. 2011.Investigation of the relationship between organic porosity and thermal maturity in the Marcellus Shale.SPE144370 North American Unconventional Gas Conference and Exhibition 14–16 June The Woodlands Texas USA.",{},{"id":24,"text":2683,"url":24,"identifiers":2684},"Milner M. 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