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Composition and Genesis of Carbonate Concretions in the Region of Paramushir Hydroacoustic Anomalies (Sea of Okhotsk) 鄂霍次克海副湖水声异常区碳酸盐结块的组成及成因
IF 0.8 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2023-05-24 DOI: 10.1134/S0024490223700104
V. V. Petrova, V. A. Rashidov, N. V. Gorkova

Carbonate concretions in the region of Paramushir hydroacoustic anomalies are confined to the methane seep zones controlled by deep (tectonically weakened) bottom areas. Based on the structure, as well as chemical and mineral composition, the concretions can be classified as volcanosedimentary rock consisting of the vitro-, litho-, and crystalloclasts and buried microfauna cemented with the carbonate (aragonite) cement. The details and sequence of mineral formation of carbonate concretions are considered.

副湖水声异常区域的碳酸盐结核局限于深部(构造弱化)底区控制的甲烷渗漏带。根据其结构、化学和矿物组成,可将其分类为火山沉积岩,由离体、岩屑和结晶碎屑组成,埋藏的微动物群以碳酸盐(文石)胶结物胶结。研究了碳酸盐结核矿物形成的细节和顺序。
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引用次数: 0
New Data on the Age of the Ozernoe Polymetallic Deposit (Western Transbaikalia) 外贝加尔湖西部Ozernoe多金属矿床时代的新资料
IF 0.8 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2023-05-24 DOI: 10.1134/S0024490223700074
O. R. Minina, I. V. Gordienko, B. B. Damdinov, V. S. Tashlykov, T. A. Goneger, V. S. Skripnikov, V. S. Lantseva, V. B. Khubanov, E. V. Kislov

The article presents results of the biostratigraphic and U–Pb geochronological (detrital zircon) studies of the volcanoterrigenous lacustrine member of the upper subformation (Lower Paleozoic Oldynda Formation), which contains polymetallic massive sulfide ores of the Ozernoe deposit (Kurba–Eravna ore district, western Transbaikalia). The first, second, and “crystalline tuff” horizons of the first ore-bearing level of the Ozernaya member were studied. It is represented by an alternation of tuffs, calcareous, siliceous, carbonaceous tuffites, pelitomorphic limestones, calcareous gravelstones with interlayers and lenses of mineralized tuffaceous conglobreccia and layers of banded siderite pyrite ores. For the first time, bryozoans, algae, and palynoflora were recorded in calcareous tuffaceous siltstones and limestones of the second and “crystalline tuff” productive horizons. These data indicate the Early Carboniferous (Tournaisian) time of sediment accumulation. Results of the U–Pb geochronological studies of detrital zircons from the mineralized tuffaceous conglobreccia of the third productive horizon suggest that the lower boundary of rock formation is not older than Late Cambrian.

本文介绍了外贝加尔西部Kurba-Eravna矿区Ozernoe矿床上亚组(下古生界Oldynda组)火山陆源湖段含多金属块状硫化物矿石的生物地层学和U-Pb年代学(碎屑锆石)研究结果。对奥泽纳亚段一含矿层的第一、第二和“结晶凝灰岩”层位进行了研究。以凝灰岩、钙质、硅质、碳质凝灰岩、泥晶灰岩、钙质砾石、矿化凝灰质长角砾岩的夹层和透镜体以及带状菱铁矿黄铁矿矿石层为代表。苔藓虫、藻类和孢粉植物首次被记录在第二和“结晶凝灰岩”生产层的钙质凝灰岩粉砂岩和石灰石中。这些资料反映了早石炭世(图尔奈世)沉积的时代。对第三产层矿化凝灰质砾岩碎屑锆石的U-Pb年代学研究结果表明,地层下界年龄不超过晚寒武世。
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引用次数: 1
Chemical Weathering Indexes: Implication for Paleoclimatic Reconstructions, with the Vendian–Lower Cambrian Section of Podolian Transnistria as Example 化学风化指标对古气候重建的意义——以波多利亚河德涅斯特河文第—下寒武统剖面为例
IF 0.8 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2023-05-24 DOI: 10.1134/S0024490222700043
A. V. Maslov, V. N. Podkovyrov

The article provides an overview of various indexes/indicators (Vogt, Parker, CIA, CIW, PIA, MIA, and others) used for studying weathering profiles/crusts and reconstructing paleoclimatic environments of sedimentary sequence accumulation. Their possibilities are demonstrated with Vendian–Lower Cambrian terrigenous rocks of Podolian Transnistria (southwestern slope of the Ukrainian Shield) as example. Distribution of index ba1 values in this section indicates the presence of material subjected to intense transformation during the chemical weathering in mudstones of the Nagoryany Formation, the lower part of the Danilovka and the middle part of the Studenitsa formations. For mudstones of the Danilovka–Zbruch interval, the HM values are close to the HMPAAS. The HM values are slightly higher for rocks of the Yaryshev–Nagoryany interval and comparable to those inherent in hot tropical continental clays for mudstones in the lower part of the Yaryshev Formation. Average value of index SA for mudstones of the entire section is 5.6 ± 0.7. Mudstones of the Grushka–Nagoryany interval, where SA < SAPAAS, are composed of a more weathered material. The WIP values in mudstones of the Mogilev and Yaryshev formations, as well as in the upper part of the Zbruch Formation, correspond to the interval of their values between the PAAS and average Archean granite. Clay rocks of other formations have WIP ≤ WIPPAAS. Average CIA value (71 ± 4) for mudstones virtually corresponds to the CIA value (70), which separates the sediments of cold/arid and warm/humid climates. Variations in the index CIW value along the section are oriented similarly as CIA variation. The vast majority of mudstones are characterized by PIA > PIAPAAS. The average CPA value is 91 ± 4, which is also typical for PAAS. These and other data suggest the following point: based on a “direct” interpretation of the values of various chemical weathering indexes inherent in the fine-grained clastic rocks, paleoclimate in Podolian Transnistria was rather moderate or warm humid in the Vendian‒Early Cambrian. Comparison of the CIA values of mudstones with the values for the particulate suspended matter in modern rivers suggests that the Vendian‒Early Cambrian climate resembled the dry and humid subtropical or dry tropical type with elements of the humid climate.

本文综述了用于研究风化剖面/壳、重建沉积层序聚集古气候环境的各种指标/指标(Vogt、Parker、CIA、CIW、PIA、MIA等)。以乌克兰地盾西南坡波多利亚德涅斯特河沿岸的文第—下寒武统陆源岩石为例,证明了这种可能性。该剖面ba1指数的分布表明,在Nagoryany组、Danilovka组下部和Studenitsa组中部的泥岩中存在化学风化过程中发生强烈转化的物质。对于Danilovka-Zbruch段泥岩,HM值与HMPAAS值接近。亚里舍夫—纳格里亚尼段岩石的HM值略高,与亚里舍夫组下部泥岩的热带大陆粘土固有HM值相当。整个剖面泥岩的SA指数平均值为5.6±0.7。Grushka-Nagoryany段泥岩,其中SA <SAPAAS是由更风化的材料组成的。Mogilev组和Yaryshev组以及Zbruch组上部泥岩的WIP值与PAAS和平均太古宙花岗岩之间的区间相对应。其他地层粘土岩的WIP≤WIPPAAS。泥岩的平均CIA值(71±4)与CIA值(70)基本一致,区分了冷/干旱和暖/湿润气候的沉积物。指数CIW值沿剖面的变化方向与CIA变化方向相似。绝大多数泥岩具有PIA >PIAPAAS。平均CPA值为91±4,这也是典型的PAAS。通过对细粒碎屑岩中各种化学风化指标的“直接”解释,可以得出文德—早寒武纪波多利亚德涅斯特河沿岸的古气候较为温和或温暖湿润。泥岩的CIA值与现代河流中颗粒悬浮物的CIA值的比较表明,文第—早寒武世气候类似于干燥湿润的亚热带或干燥的热带气候,具有湿润气候的要素。
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引用次数: 1
Flat Spots within Cenozoic Sediments of the Nansen Basin, Arctic Ocean: Indicators for Serpentinization, Gas Generation and Accumulation Processes 北冰洋南森盆地新生代沉积物中的扁平点:蛇纹岩作用、生气和成藏过程的标志
IF 0.8 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2023-04-18 DOI: 10.1134/S0024490222060074
S. Yu. Sokolov, W. H. Geissler, A. S. Abramova, D. A. Ryzhova, I. S. Patina

Flat spot anomalies in the Quaternary part of the section of the Nansen Basin are imaged in seismic records and are interpreted to be related to gas-rich fluid accumulations. The flat spots are mainly located above basement highs between magnetic spreading anomalies C20 (~43 Ma) and C12 (~33 Ma). The complex morphometric analysis of flat spots show that serpentinization processes identified from modelling of gravity anomalies could be original gas source. This process also makes smoothing of the basement highs amplitudes. The depth of the top of the flat spots below the seafloor has an almost constant value of ~390 m indicating the ascent of gases from variable basement depths to a common subsurface fluid trap. The depth of the anomalies below the seafloor corresponds to a theoretical thickness of gas hydrate stability zone in the studied region. Gravity modeling along the Arktika-2011-03 section showed the position of the upper mantle blocks with lower (to 2.95 g/cm3) density within the highs of the acoustic basement. The flat spot anomalies occur above basement highs, below which blocks with lower density typical of serpentinized rocks are modelled. Thus, the serpentinization of the upper mantle ultramafic rocks is considered a main geochemical process, which can explain generation and accumulation of gas in oceanic abyss at a 1–3 km thick sedimentary cover, as well as small vertical movements of the basement blocks due to density reduction and expansion of serpentinized rock.

南森盆地第四纪剖面的平斑异常在地震记录中被成像,并被解释为与富气流体聚集有关。扁斑主要位于磁展异常C20 (~43 Ma)和C12 (~33 Ma)之间的基底高点上方。平坦点的复杂形态计量学分析表明,重力异常模拟识别的蛇纹石化过程可能是原始气源。这个过程也使基底高振幅平滑。海底以下平坦点顶部的深度几乎是恒定的~390 m,表明气体从不同的基底深度上升到一个常见的地下流体圈闭。海底以下异常深度对应于研究区天然气水合物稳定带的理论厚度。沿Arktika-2011-03剖面的重力模拟显示,密度较低(至2.95 g/cm3)的上地幔块体位于声波基底的高点。平斑异常出现在基底高地之上,在基底高地之下,模拟了典型蛇纹岩密度较低的块体。因此,上地幔超基性岩的蛇纹石化作用被认为是一个主要的地球化学过程,它可以解释1-3 km厚沉积盖层海洋深渊中天然气的生成和聚集,以及由于蛇纹石化岩石密度降低和膨胀导致基底块体的小幅度垂直运动。
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引用次数: 0
Adsorption of Rare Earth Metal Cations by Base Metal Sulfides in the Broken Spur and TAG Hydrothermal Fields, Atlantic Ocean 贱金属硫化物在大西洋断刺和TAG热液中对稀土金属阳离子的吸附
IF 0.8 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2023-04-18 DOI: 10.1134/S0024490223010066
G. V. Novikov, N. V. Lobus, N. A. Shulga, O. Yu. Bogdanova

The article presents the results of sorption of rare earth metal (REM) cations on samples of deep-sea base metal sulfides in the Broken Spur and TAG hydrothermal fields (Mid-Atlantic Ridge). The studied samples contain the following major minerals: marcasite, pyrrhotite, pyrite, and sphalerite in the Broken Spur field; chalcopyrite, pyrite, and marcasite in the TAG field. It has been established that these Fe–Cu–Zn sulfide minerals are natural absorbents. The exchange capacity of sulfide minerals for REM cations is 0.006‒0.061 mg-equiv/g. The exchange complex of sulfide minerals comprises the cations of alkaline, alkali-earth metals, and main cations of metals in the crystal lattice – Fe, Zn, Cu (in very limited quantities). The mechanism of the REM cation absorption is ion-exchange equivalent to the exchange cations of sulfide minerals. It was found that REM cations occur in the sulfide minerals almost completely in the sorbed form (more than 90% of the total amount). Apparently, the chemically bound form is possible only for Lu and Dy cations. The mineral composition of sulfide deposits is preserved in the exchange reaction products, and new phases do not appear.

本文介绍了中大西洋洋脊破碎冲和TAG热液区深海贱金属硫化物样品对稀土金属(REM)阳离子的吸附结果。研究样品中主要矿物有:破碎直冲矿区的黄铁矿、磁黄铁矿、黄铁矿和闪锌矿;黄铜矿,黄铁矿和黄铁矿在TAG领域。这些铁、铜、锌硫化物矿物是天然的吸附剂。硫化物矿物对REM阳离子的交换容量为0.006 ~ 0.061 mg-当量/g。硫化矿物的交换配合物包括碱性、碱土金属的阳离子,以及晶格中金属的主要阳离子——铁、锌、铜(数量非常有限)。REM阳离子吸收的机理是与硫化物矿物交换阳离子等效的离子交换。研究发现,快速动眼期阳离子几乎全部以吸附形式存在于硫化矿物中(占总量的90%以上)。显然,化学结合的形式只可能存在于Lu和Dy阳离子。硫化物矿床的矿物组成保存在交换反应产物中,不出现新的相。
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引用次数: 0
Influence of L.V. Pustovalov’s Works on the Development of Petroleum Lithology 普斯托瓦洛夫著作对石油岩性学发展的影响
IF 0.8 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2023-04-18 DOI: 10.1134/S0024490222700018
V. G. Kuznetsov, A. N. Dmitrievsky

The article discusses the main directions of lithological studies in the oil-and-gas geology, continuing and developing the ideas and researches of L.V. Pustovalov. Several such studies are coordinated closely with other geological branches (tectonics, stratigraphy, and others). A wide range of such studies is devoted to analysis of the structure and development of sedimentary basins; elucidation of the structure of the internal structure of sedimentary complexes; prediction and prospecting for non-structural oil-and-gas traps; and study of natural oil-and-gas reservoirs at different hierarchical levels.

本文论述了油气地质中岩性研究的主要方向,继承和发展了普斯托瓦洛夫的思想和研究。一些这样的研究与其他地质学分支(构造学、地层学等)密切配合。这类研究的范围广泛,致力于分析沉积盆地的构造和发育;沉积杂合体内部构造的构造解析非构造油气圈闭预测与勘探并对不同层次的天然油气藏进行了研究。
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引用次数: 0
Globular Phyllosilicates of the Glauconite–Illite Series in the Cambrian and Ordovician Rocks of the Eastern Baltica (Northern Estonia, Western Lithuania, and Western Latvia) 波罗的海东部(爱沙尼亚北部、立陶宛西部和拉脱维亚西部)寒武系和奥陶系海绿石-伊利石系列中的球状层状硅酸盐
IF 0.8 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2023-04-18 DOI: 10.1134/S002449022270002X
T. A. Ivanovskaya, B. A. Sakharov, T. S. Zaitseva

The mineralogical, structural and crystal-chemical features of seven samples of globular phyllosilicates of the glauconite–illite series (GPS) from the Lower Cambrian sequences of Northern Estonia and Western Lithuania, from the Middle Cambrian sequences of Western Latvia, and also from the Lower Ordovician sequences of Northern Estonia and Western Latvia are considered for the first time. Based on Al index (KAl = VIAl/[VIFe3+ + VIAl]) varying from 0.27 to 0.59, the globular phyllosilicates are attributed to the glauconite–illite series, most of which are represented by glauconites (the Al index is KAl = 0.27–0.46) and one sample, by Al-glauconite (KAl = 0.59). The K2O content in minerals is from 7.12 to 7.90%. The content of expandable layers (4–13%), their types (smectite, vermiculite), and the character of their alternation (R = 0, R = 2) were determined for the first time in the studied samples by simulation of experimental X-ray diffraction patterns from oriented specimens. Simulation of X-ray diffraction patterns obtained from unoriented specimens made it possible to determine the degree of three-dimensional order and mean values of the unit-cell parameter b (9.056–9.094 Å), as well as the distribution of their individual micaceous varieties. Based on these data, the microheterogeneity of the Cambrian and Ordovician GPSs was established and compared with the heterogeneity in the previously studied Riphean GPS (Drits et al., 2013). The obtained Rb-Sr и K‑Ar ages for the studied Middle Cambrian and Lower Ordovician samples, as well as the earlier published dates for the Lower Cambrian samples, are “rejuvenated” relative to age limits accepted for the Cambrian and Lower Ordovician (Gradstein et al., 2020). The relationship of the Cambrian and Lower Ordovician “rejuvenated” isotopic dates and the discovered GPS heterogeneity, as well as possible reasons for its occurrence, are discussed.

本文首次研究了爱沙尼亚北部和立陶宛西部下寒武统层序、拉脱维亚西部中寒武统层序以及爱沙尼亚北部和拉脱维亚西部下奥陶统层序海绿石-伊立石系列(GPS)的7个球状层状硅酸盐样品的矿物学、结构和晶体化学特征。从Al指数(KAl = VIAl/[VIFe3+ + VIAl])在0.27 ~ 0.59之间的变化来看,球状层状硅酸盐属于海绿石—伊利石系列,其中大部分为海绿石(Al指数为KAl = 0.27 ~ 0.46),有一个样品为Al-海绿石(KAl = 0.59)。矿物中K2O含量为7.12% ~ 7.90%。通过模拟取向试样的实验x射线衍射图,首次测定了试样中可膨胀层的含量(4 ~ 13%)、类型(蒙脱石、蛭石)及其变化特征(R = 0, R = 2)。模拟无取向样品的x射线衍射图,可以确定三维有序程度和单位胞参数b (9.056-9.094 Å)的平均值,以及它们的单个云母品种的分布。基于这些数据,建立了寒武系和奥陶系GPS的微观非均质性,并与之前研究的Riphean GPS的非均质性进行了比较(Drits et al., 2013)。所研究的中寒武统和下奥陶统样品的Rb-Sr - K - Ar年龄,以及之前公布的下寒武统样品的年龄,相对于寒武统和下奥陶统的公认年龄限制,都得到了“恢复”(Gradstein et al., 2020)。讨论了寒武系和下奥陶统“返青”同位素日期与GPS非均质性的关系及其可能的原因。
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引用次数: 0
Chemical Composition of Sediments and Its Changes at the Modern Hydrothermal System Center in the Middle Valley, Juan de Fuca Ridge, Hole 858B ODP Juan de Fuca Ridge 858B孔ODP中部山谷现代热液系统中心沉积物化学成分及其变化
IF 0.8 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2023-04-18 DOI: 10.1134/S0024490223010030
V. B. Kurnosov, Yu. I. Konovalov, K. R. Galin

The article presents the results of studying changes in the chemical composition of Pleistocene sediments from Hole 858B (depth 38.6 m, temperature gradient 10‒11°C/m) drilled in the Middle Valley, Juan de Fuca mid-ocean ridge (Northeast Pacific) in the Dead Dog hydrothermal field 20 m away from a “black smoker” (temperature 276°C). The content of macroelements in these sediments was studied by the XRD method. For the first time, data on a large set of trace elements were obtained from this object using the ICP-MS method. The chemical composition of sediments changed in the process of solution–sediment interaction during a rapid downsection increase of temperature. In the upper part of Sequence I (1.97‒10.41 m), the sediments are commonly altered slightly at a temperature of about 17°C. Changes in the content of macro- and trace elements are prominent in the lower part of Sequence I (12.70‒25.31 m, average temperature 112‒197°C). The chemical composition of sediments is most altered in Sequences IIB and IID (25.31‒38.6 m, temperature from 112‒197 to 320‒330°С). Changes in the content of the majority of macro- and trace elements in the sediments of Sequences IIB and IID are similar, except for a stronger decrease of chemical elements in the sediments of Sequence IID, which is marked by a significantly lower content of Cu, Zn, Ga, Rb, Sr, Ag, Cd, Sb, Cs, Ba, Tl, and Bi (i.e., the majority of detected elements except U) than in background sediments. Sediments in Sequence IID, as in Sequence IIB, contain less Ca, Na, K, and P, but more Mg. A lower content of the above-listed elements in these sediments can be attributed to their evacuation during the solution–sediment interaction and concentration in the solution, whereas a higher content of these elements is likely related to their input into sediments from the solution and, accordingly, their depletion in the solution. The results of studying the chemical composition of metalliferous sediments (Sequence III, 0‒1.97 m) and sulfide layer IV (10.41‒12.70 m), as well as the chemical composition of unaltered background sediments from Holes 855A, 855C, and 855D are presented.

本文介绍了在离“黑烟炉”(温度276℃)20 m的Dead Dog热液区Juan de Fuca洋中脊Middle Valley(东北太平洋)钻探的858B孔(深度38.6 m,温度梯度10-11℃/m)更新世沉积物化学成分变化的研究结果。采用x射线衍射(XRD)分析了这些沉积物中微量元素的含量。首次用ICP-MS法测定了该样品的大量微量元素。在温度快速下降的过程中,沉积物的化学成分发生了变化。层序ⅰ上部(1.97 ~ 10.41 m)温度约为17℃,沉积物普遍发生轻微变化。序列1下部(12.70 ~ 25.31 m,平均温度112 ~ 197℃)宏量元素和微量元素含量变化明显。IIB和IID层序(25.31 ~ 38.6 m,温度范围112 ~ 197 ~ 320 ~ 330°С)沉积物化学成分变化最大。IIB序列和IID序列沉积物中大部分常量元素和微量元素含量变化相似,但IID序列沉积物中化学元素含量下降更强,Cu、Zn、Ga、Rb、Sr、Ag、Cd、Sb、Cs、Ba、Tl和Bi(即除U外的大部分检测元素)含量明显低于背景沉积物。层序IID的沉积物与层序IIB一样,Ca、Na、K和P含量较低,而Mg含量较高。这些沉积物中上述元素的含量较低,可归因于它们在溶液-沉积物相互作用过程中被排出,以及在溶液中的浓度,而这些元素的含量较高,可能与它们从溶液中输入到沉积物中有关,因此,它们在溶液中耗尽。给出了含金属沉积物(层序III, 0 ~ 1.97 m)和硫化物层IV (10.41 ~ 12.70 m)的化学组成研究结果,以及855A、855C和855D孔未改变背景沉积物的化学组成。
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引用次数: 0
C and O Isotope Composition of the Neoproterozoic Pre-, Syn-, and Postglacial Carbonates: Evidence from the Longdor Uplift and Western Slope of the Aldan Shield, Southern Siberian Platform 新元古代冰期前、冰期新、冰期后碳酸盐的C、O同位素组成:来自南西伯利亚地台Aldan盾西斜坡隆多隆起的证据
IF 0.8 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2023-04-18 DOI: 10.1134/S0024490222700055
A. V. Shatsillo, S. V. Rud’ko, I. V. Latysheva, B. G. Pokrovsky, D. V. Rud’ko, I. V. Fedyukin, A. B. Kuznetsov

New data on the C and O isotope composition in the Neoproterozoic carbonates of the Ballaganakh and Dal’nyaya Taiga regional stages (southeastern margin of the Patom paleobasin (hereafter, Basin) are presented. The negative δ13С anomaly, established in the upper part of the Ballaganakh regional stage, is comparable (in amplitude and stratigraphic position) to the Trezona anomaly, which preceded the Marinoan glaciation. The carbonate layers in glacial deposits of the Nichatka Formation of the Dal’nyaya Taiga regional stage have moderately positive δ13С values. The dolomite unit at the postglacial sequence base is characterized by moderately negative δ13С values that are typical for the cap carbonate sequence associated with the end-Marinoan glaciation. The lower part of the postglacial sequence (Barakun Formation) is characterized by a gradual increase of calcite in the carbonate component of rocks and a shift in the isotope composition corresponding to the difference in the fractionation coefficient of stable C and O isotopes for dolomite and calcite. This phenomenon, recorded in the postglacial sequences of Namibia and Canada as well, indicates that the carbonate mineral composition was governed by a global change in water chemistry rather than postsedimentary alteration. The overlying carbonate rocks of the Dal’nyaya Taiga regional stage in the epicontinental part of the Patom Basin (Sen Formation) are depleted in 13С compared to their shelf analogs in the Ura Uplift. Probably, the carbonates were accumulated asynchronously in the epicontinental and shelf facies of the Patom Basin. The reconstructed trend of variations in the carbon isotope composition for the Dal’nyaya Taiga regional stage is characterized by positive and low-amplitude negative δ13С anomalies similar to those in the Doushantuo Formation (China).

本文报道了巴拉甘akh和Dal 'nyaya Taiga区域阶段(Patom古盆地东南缘)新元古代碳酸盐岩C、O同位素组成的新资料。负δ13С异常建立于巴拉干纳克区域阶段的上部,在振幅和地层位置上与马里诺冰期之前的Trezona异常相当。达尔尼雅针叶林区域期Nichatka组冰川沉积碳酸盐层具有中等正δ13С值。冰后层序基底处的白云岩单元具有中等负δ13С值的特征,这是与马里诺末冰期相关的盖层碳酸盐岩层序的典型特征。冰后层序下部(Barakun组)岩石碳酸盐组分中方解石含量逐渐增加,其同位素组成发生偏移,对应于白云石和方解石稳定C、O同位素分馏系数的差异。在纳米比亚和加拿大的冰川后序列中也记录了这种现象,表明碳酸盐矿物组成是由全球水化学变化而不是沉积后的蚀变所控制的。与乌拉隆起的陆架类似物相比,在13С中,Patom盆地陆表部分(Sen组)Dal 'nyaya Taiga区域阶段的上覆碳酸盐岩已经枯竭。在Patom盆地陆表相和陆架相中,碳酸盐岩可能是不同步聚集的。达尔尼雅针叶林区域阶段碳同位素组成变化的重建趋势表现为与中国陡山沱组相似的正、低振幅负δ13С异常。
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引用次数: 0
Are There Restrictions Related to the Presence of Land Plants for Reconstructing Rivers of Different Categories? 不同类型河流改造中陆生植物的存在是否有限制?
IF 0.8 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2023-04-18 DOI: 10.1134/S0024490223010054
A. V. Maslov, O. Yu. Melnichuk

The article analyzes the distribution of datapoints of individual and averaged mudstones samples from almost 40 sedimentary successions of the Neoproterozoic–Ordovician (epoch lacking land plants) and the Devonian–Holocene (time of the appearance and abundance of land plants—“green epoch”) in the (La/Yb)N–Eu/Eu*, (La/Yb)N–(Eu/Sm)N, and (La/Yb)N–Th diagrams with classification fields of the silty–pelitic particulate matter in the estuary of different-category modern rivers. No fundamental differences between the “green epoch” and pre-Silurian rivers were revealed. In combination with other data, the above fact suggests the following conclusion: since the terrestrial vegetation is absent (and not only in the Neoproterozoic–Ordovician), the categories of rivers, which drained different (in area and composition) catchment areas and transported the fine-grained particulate material to the shelf zones were not fundamentally different from those at present.

本文分析了新元古代—奥陶系(缺乏陆生植物的时代)和泥盆纪—全新世(陆生植物出现和丰度的时间—“绿色时代”)近40个沉积序列中单个和平均泥岩样品在(La/Yb)N - Eu/Eu*、(La/Yb)N - (Eu/Sm)N和(La/Yb)N - th图及不同类型现代河流河口粉砂质泥质颗粒分类场中的数据点分布。“绿色时代”和前志留纪河流之间没有根本的区别。结合其他资料,上述事实表明:由于陆生植被的缺失(不仅是新元古代—奥陶纪),在不同(面积和组成)集水区排水并将细粒颗粒物质输送到陆架带的河流种类与现在并没有本质上的区别。
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Lithology and Mineral Resources
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