Based on a variety of new or re-evaluated geo logica l and geophysical constraints , the following modifications to the Teniary tecton ic history of nonh-ccntral New Mexico are proposed: ( I) reverse faulting along the Pajarito fault zone defined the western boundary of a late Laramide base ment uplift (Pajarito uplift) that was contiguous with the Sangre de Cristo uplift to the east; (2) the Tijeras fault zone constitu ted a re leasing bend in the right-lateral strike-slip system of the Laramide southern Roc ky Mountains and controlled extensional subsidence within an Eocene half-graben to the nonhwest (the Gali,teo basin): (3) development of a flexural hi nge along a Laramide precursor to the Santa Ana accommodat ion zone (new name) may have faci litated the southeastward tilting of the floor of the Galisteo basin and locally delineated the sou thern boundary of the Pajarito uplift; and (4 ) the Pajari to uplift began to collapse due to extension beginning in the late Oligoceneearly Miocene, and continued subsidence and westward tilting of the resulting Espanola half-graben caused deposition of about 3 km of Santa Fe Group sediments near the Pajarito fault zone .
基于各种新的或重新评估的地质和地球物理约束条件，对新墨西哥州非中部地区的第三纪构造史进行了以下修正:(1)沿Pajarito断裂带的逆断裂确定了晚Laramide基底隆起(Pajarito隆起)的西部边界，该隆起东部与Sangre de Cristo隆起相邻;(2) Tijeras断裂带在罗克天山南缘Laramide右旋走滑体系中形成了一个大弯曲，控制了西北缘始新世半地堑(Gali,teo盆地)内的伸展沉降;(3)沿着圣安娜适应带(新名称)的Laramide前体发育的弯曲断层可能促进了加里斯托盆地底部的东南倾斜，并在局部划定了帕加里托隆起的南部边界;(4)从渐新世晚期至中新世早期开始，帕加里托隆起因伸展而开始崩塌，由此形成的Espanola半地堑持续沉降和向西倾斜，在帕加里托断裂带附近沉积了约3 km的Santa Fe群沉积物。
{"title":"Suggested revisions to the Tertiary tectonic history of north-central New Mexico","authors":"S. Cather","doi":"10.56577/ffc-43.109","DOIUrl":"https://doi.org/10.56577/ffc-43.109","url":null,"abstract":"Based on a variety of new or re-evaluated geo logica l and geophysical constraints , the following modifications to the Teniary tecton ic history of nonh-ccntral New Mexico are proposed: ( I) reverse faulting along the Pajarito fault zone defined the western boundary of a late Laramide base ment uplift (Pajarito uplift) that was contiguous with the Sangre de Cristo uplift to the east; (2) the Tijeras fault zone constitu ted a re leasing bend in the right-lateral strike-slip system of the Laramide southern Roc ky Mountains and controlled extensional subsidence within an Eocene half-graben to the nonhwest (the Gali,teo basin): (3) development of a flexural hi nge along a Laramide precursor to the Santa Ana accommodat ion zone (new name) may have faci litated the southeastward tilting of the floor of the Galisteo basin and locally delineated the sou thern boundary of the Pajarito uplift; and (4 ) the Pajari to uplift began to collapse due to extension beginning in the late Oligoceneearly Miocene, and continued subsidence and westward tilting of the resulting Espanola half-graben caused deposition of about 3 km of Santa Fe Group sediments near the Pajarito fault zone .","PeriodicalId":325871,"journal":{"name":"San Juan Basin IV","volume":"94 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"130357333","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
R. Chamberlin, James S. Harris, Margaret I. Onimole
We present a geochemical map showing the estimated silica (eSiO,) content of 496 NURE streamsediment samples collected within the Eocene San Jose Fonnation. This computer-generated map essentially shows the bulk distribution of quartz within the fonnation. The formation is clearly divisible into a central lowsilica (low quartz) domain, a western intennediate-s ilica domain and a ~outheastern high-sil ica domain. Our follow-up stream-sediment sampl ing and analys is have verified the chemical patterns seen in the NURE data. Preliminary petrographic study of follow-up stream-sedi ment samples inuicates that quartz/fe ldspar ratios are relative ly constant within each silica domain, as defined by the NURE data. Some second-order noise within silica domains apparently retlects high concentrations of mudstone grains or heavy minerals in the NURE samples . Quart z/feldspar est imates from 44 thin sections of San Jose sandstones demonstrate a good correlat ion of granite-derived arkose with the low-silica domain, cherty subarkose with the intermediate-silica domain , and subfeldspathic arenite with the high-silica domain . We interpret the intermediate-,ilica . subarkosic strata and the high-silica, subfeldspathic strata as the products of southerly flowi ng early E.ocene river systems that entered the basin near Aztec and Llaves . respectively ; these rivers appear to have joined near Cuba. Preliminary field observations and second-order geochemical patterns suggest that the low-silica, arkos ic strata represent relatively thi n deposits of a younger river system which overlies the main body of San Jose strata. Additional data are needed to accurate ly define the geometry of low-si lica arkosic strata within the San Jose Formation.
{"title":"A stream-sediment geochemical map (from NURE data) showing bulk silica distribution within the Eocene San Jose Formation, San Juan Basin, New Mexico","authors":"R. Chamberlin, James S. Harris, Margaret I. Onimole","doi":"10.56577/ffc-43.317","DOIUrl":"https://doi.org/10.56577/ffc-43.317","url":null,"abstract":"We present a geochemical map showing the estimated silica (eSiO,) content of 496 NURE streamsediment samples collected within the Eocene San Jose Fonnation. This computer-generated map essentially shows the bulk distribution of quartz within the fonnation. The formation is clearly divisible into a central lowsilica (low quartz) domain, a western intennediate-s ilica domain and a ~outheastern high-sil ica domain. Our follow-up stream-sediment sampl ing and analys is have verified the chemical patterns seen in the NURE data. Preliminary petrographic study of follow-up stream-sedi ment samples inuicates that quartz/fe ldspar ratios are relative ly constant within each silica domain, as defined by the NURE data. Some second-order noise within silica domains apparently retlects high concentrations of mudstone grains or heavy minerals in the NURE samples . Quart z/feldspar est imates from 44 thin sections of San Jose sandstones demonstrate a good correlat ion of granite-derived arkose with the low-silica domain, cherty subarkose with the intermediate-silica domain , and subfeldspathic arenite with the high-silica domain . We interpret the intermediate-,ilica . subarkosic strata and the high-silica, subfeldspathic strata as the products of southerly flowi ng early E.ocene river systems that entered the basin near Aztec and Llaves . respectively ; these rivers appear to have joined near Cuba. Preliminary field observations and second-order geochemical patterns suggest that the low-silica, arkos ic strata represent relatively thi n deposits of a younger river system which overlies the main body of San Jose strata. Additional data are needed to accurate ly define the geometry of low-si lica arkosic strata within the San Jose Formation.","PeriodicalId":325871,"journal":{"name":"San Juan Basin IV","volume":"14 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"128872197","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
-Metacypris todilroensis Swain, 1946, should be reassigned to the genus Cytheridel/a Daday, I 905, to accommodate it better in the current organization of the Limnocytheridae. This placement is based on muscle scar structure, the single sulcus and close similarity of surface ornamentation. This species represents an important link between the ancestral Lutkevichinella faunas of the Triassic and the extant genus Cwheridella. The occurrence of this ostracode in the saline to hypersaline Todilto environments can be understood in terms of readaptation of a brackish-water ostracode group and perhaps in the possible parthenogenic nature of this species.
-Metacypris todilroensis Swain, 1946，应重新分配到Cytheridel属/a Daday, I 905，以更好地适应目前的Limnocytheridae组织。这种位置是基于肌肉疤痕结构，单一沟和表面纹饰的密切相似。该种代表了三叠纪祖先Lutkevichinella动物群与现存的Cwheridella属之间的重要联系。这种介形虫出现在咸水到高咸水的Todilto环境中，可以从微咸水介形虫群的重新适应和该物种可能的单性生殖性质来理解。
{"title":"Reassignment of the Jurassic Todilto Limestone Ostocode Metacypris Todiltoensis Swain 1946, to Cytheridella, with notes on the phylogeny and environmental implications of this Ostracode","authors":"K. Kietzke","doi":"10.56577/ffc-43.173","DOIUrl":"https://doi.org/10.56577/ffc-43.173","url":null,"abstract":"-Metacypris todilroensis Swain, 1946, should be reassigned to the genus Cytheridel/a Daday, I 905, to accommodate it better in the current organization of the Limnocytheridae. This placement is based on muscle scar structure, the single sulcus and close similarity of surface ornamentation. This species represents an important link between the ancestral Lutkevichinella faunas of the Triassic and the extant genus Cwheridella. The occurrence of this ostracode in the saline to hypersaline Todilto environments can be understood in terms of readaptation of a brackish-water ostracode group and perhaps in the possible parthenogenic nature of this species.","PeriodicalId":325871,"journal":{"name":"San Juan Basin IV","volume":"4 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"115179424","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
---- Campanian-Maastrichtian nonmartne strata of the San Juan Basin pertain to the Fruitland Formation and the Kirtland Formation. The Kirtland consists, in ascending order, of the Bisti, Hunter Wash, Farmington. De-na-zin and Naashoibito Members. The Fruitland is dominantly of deltaic and paludal origin and the Kirtland is of broadly fluvial origin. The Bisti Member is a gas reservoir. The majority of fossil vertebrates are from an interval in the uppermost Fruitland and from the Naashoibito Member. Distinct vertebrate and invertebrate faunas and floras can be distinguished for the Fruitland, pre-Naashoibito Kirtland and Naashoibito. Diverse evidence indicates that the Fruitland is of Judithian (late Campanian) age, the pre-Naashoibito Kirtland is of Edmontonian (early Maastrichtian) age and the Naashoibito is of Lancian (late Maastrichtian) age. There is no large-scale angular unconformity at the base of the Ojo Alamo Sandstone.
{"title":"Stratigraphy, paleontology and age of the Fruitland and Kirtland Formations (Upper Cretaceous), San Juan Basin, New Mexico","authors":"A. Hunt, S. Lucas","doi":"10.56577/ffc-43.217","DOIUrl":"https://doi.org/10.56577/ffc-43.217","url":null,"abstract":"---- Campanian-Maastrichtian nonmartne strata of the San Juan Basin pertain to the Fruitland Formation and the Kirtland Formation. The Kirtland consists, in ascending order, of the Bisti, Hunter Wash, Farmington. De-na-zin and Naashoibito Members. The Fruitland is dominantly of deltaic and paludal origin and the Kirtland is of broadly fluvial origin. The Bisti Member is a gas reservoir. The majority of fossil vertebrates are from an interval in the uppermost Fruitland and from the Naashoibito Member. Distinct vertebrate and invertebrate faunas and floras can be distinguished for the Fruitland, pre-Naashoibito Kirtland and Naashoibito. Diverse evidence indicates that the Fruitland is of Judithian (late Campanian) age, the pre-Naashoibito Kirtland is of Edmontonian (early Maastrichtian) age and the Naashoibito is of Lancian (late Maastrichtian) age. There is no large-scale angular unconformity at the base of the Ojo Alamo Sandstone.","PeriodicalId":325871,"journal":{"name":"San Juan Basin IV","volume":"86 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"133028266","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
A meander loop of the upper Rio Puerco of the east experienced a neck cutoff during the late winter-early spring of 1988, temporarily changing the gradient of the stream from 0.003 (m/m) to 0.25 . Observations before, during and after the cutoff document (I) that cutoff was not a major disruption for the stream, (2) that timing, order and duration of events are important in crossing geomorphic thresholds and subsequent adjustments, (3) that the threshold for cutoff was lowered considerably by erosion and humans in preceding years, (4) that breaching was thwarted temporarily by low-flow processes, (5) that initial breaching took place during moderate flow, and (6) that subsequent large flows in 1988 caused both width and gradient to be fully adjusted with upstream and downstream values within one flow season. The steep gradient of the breach did not propagate upstream as a headwall; rather the slope increased slightly upstream and extended until the former gradient was reached.
{"title":"Rapid adjustment of the Rio Puerco to meander cutoff: Implications for effective geomorphic processes, crossing thresholds and timing of events.","authors":"D. Love","doi":"10.56577/ffc-43.399","DOIUrl":"https://doi.org/10.56577/ffc-43.399","url":null,"abstract":"A meander loop of the upper Rio Puerco of the east experienced a neck cutoff during the late winter-early spring of 1988, temporarily changing the gradient of the stream from 0.003 (m/m) to 0.25 . Observations before, during and after the cutoff document (I) that cutoff was not a major disruption for the stream, (2) that timing, order and duration of events are important in crossing geomorphic thresholds and subsequent adjustments, (3) that the threshold for cutoff was lowered considerably by erosion and humans in preceding years, (4) that breaching was thwarted temporarily by low-flow processes, (5) that initial breaching took place during moderate flow, and (6) that subsequent large flows in 1988 caused both width and gradient to be fully adjusted with upstream and downstream values within one flow season. The steep gradient of the breach did not propagate upstream as a headwall; rather the slope increased slightly upstream and extended until the former gradient was reached.","PeriodicalId":325871,"journal":{"name":"San Juan Basin IV","volume":"40 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"121122981","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico.
{"title":"Supplemental road log 3: From Durango, Colorado to Pinyon Mesa and the Bluffs south of the San Juan River near Farmington","authors":"S. Lucas, T. Williamson","doi":"10.56577/ffc-43.73","DOIUrl":"https://doi.org/10.56577/ffc-43.73","url":null,"abstract":"Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico.","PeriodicalId":325871,"journal":{"name":"San Juan Basin IV","volume":"19 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"127034606","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
A large gap exists in our knowledge of the Pleistocene and Holocene cultural and faunal record in the San Juan Basin. Information concerning the activities of Paleo-Indians in the basin is often based on inference from other areas. Evidence found elsewhere suggests that they exploited large migratory herds of now extinct megafauna (e.g., mammoth. horse . bison and camel) . Additionally, the paleontological record of the Pleistocene and Holocene is virtually nonexistent. Some evidence suggests that mammoth. horse, elk. bighorn sheep, pronghorn antelope and muskox were the major herbivores present in the basin during th is period. The physiographic and environmental nature of the basin allowed access and exploitation of the forage resources to these an imals and apparently restricted access to bison. Traditional thinking about the lifeways of the Paleo-Indians that lived in the basin should be re-examined and founded on different research methodology before we can fully understand the story of these early human migrants and their relationship to the environment. Interdisciplinary and interagency cooperation is a cri tical factor in developing a basis for our understand ing of past life in the San Juan Basin.
{"title":"Paleo-Indians in the San Juan Basin: A paleontological perspective","authors":"F. O’Neill","doi":"10.56577/ffc-43.333","DOIUrl":"https://doi.org/10.56577/ffc-43.333","url":null,"abstract":"A large gap exists in our knowledge of the Pleistocene and Holocene cultural and faunal record in the San Juan Basin. Information concerning the activities of Paleo-Indians in the basin is often based on inference from other areas. Evidence found elsewhere suggests that they exploited large migratory herds of now extinct megafauna (e.g., mammoth. horse . bison and camel) . Additionally, the paleontological record of the Pleistocene and Holocene is virtually nonexistent. Some evidence suggests that mammoth. horse, elk. bighorn sheep, pronghorn antelope and muskox were the major herbivores present in the basin during th is period. The physiographic and environmental nature of the basin allowed access and exploitation of the forage resources to these an imals and apparently restricted access to bison. Traditional thinking about the lifeways of the Paleo-Indians that lived in the basin should be re-examined and founded on different research methodology before we can fully understand the story of these early human migrants and their relationship to the environment. Interdisciplinary and interagency cooperation is a cri tical factor in developing a basis for our understand ing of past life in the San Juan Basin.","PeriodicalId":325871,"journal":{"name":"San Juan Basin IV","volume":"14 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"126678417","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Hydrocarbon potential and stratigraphy of the Pictured Cliffs, Fruitland and Ojo Alamo Formations in the northeastern San Juan Basin.","authors":"W. F. Hoppe","doi":"10.56577/ffc-43.359","DOIUrl":"https://doi.org/10.56577/ffc-43.359","url":null,"abstract":"","PeriodicalId":325871,"journal":{"name":"San Juan Basin IV","volume":"26 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"131965157","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
-In the Upper Cretaceous Point Lookout Sandstone in southwestern Colorado, the presence of distinctly different scales of transgressive deposits defines a hierarchy of high-frequency, nearshore-marine transgressive-regressive cycles. The two cycle scales, parasequences and parasequence sets, are delineated on the basis of thickness and lithologic characteristics of the transgressive deposits at inner-shelf and back-barrier positions. This observation is contrary to most previous work on cycles at this scale, which suggests that the stratigraphic record is composed of regressive strata with the transgressive portion of the cycle being represented only by a surface of erosion or nondeposition. Here, we recognize that both regressive and transgressive deposits are important components of the cycle stratigraphy.
{"title":"Parasequence geometry and facies architecture in the upper Cretaceous Point Lookout Sandstone, Four Corners platform, southwestern Colorado","authors":"Danny R. Katzman, R. Wright-Dunbar","doi":"10.56577/ffc-43.187","DOIUrl":"https://doi.org/10.56577/ffc-43.187","url":null,"abstract":"-In the Upper Cretaceous Point Lookout Sandstone in southwestern Colorado, the presence of distinctly different scales of transgressive deposits defines a hierarchy of high-frequency, nearshore-marine transgressive-regressive cycles. The two cycle scales, parasequences and parasequence sets, are delineated on the basis of thickness and lithologic characteristics of the transgressive deposits at inner-shelf and back-barrier positions. This observation is contrary to most previous work on cycles at this scale, which suggests that the stratigraphic record is composed of regressive strata with the transgressive portion of the cycle being represented only by a surface of erosion or nondeposition. Here, we recognize that both regressive and transgressive deposits are important components of the cycle stratigraphy.","PeriodicalId":325871,"journal":{"name":"San Juan Basin IV","volume":"1 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"121399788","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Sequence stratigraphy in ramp settings--With application to upper Cretaceous rocks in the San Juan Basin","authors":"D. Nummedal","doi":"10.56577/ffc-43.185","DOIUrl":"https://doi.org/10.56577/ffc-43.185","url":null,"abstract":"","PeriodicalId":325871,"journal":{"name":"San Juan Basin IV","volume":"39 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"131847742","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
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