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Categories of Rivers that Formed Vendian and Lower Cambrian Sedimentary Sequences, Western Part of the East European Platform: Evidence from Lithogeochemistry 形成东欧地台西部文地宙和下寒武统沉积层序的河流类别:岩石地球化学证据
IF 0.7 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2024-03-02 DOI: 10.1134/S0024490223700414
A. V. Maslov, V. N. Podkovyrov

Based on lithogeochemical data related to the fine-grained clastic rocks of the Volyn, Valdai, and Baltic groups in the western part of the East European Platform (Belarus and Volyn, partly Lithuania), categories of rivers that transported the fine-grained aluminosiliciclastics to the sinks were reconstructed. It is concluded that the formation of Vendian and Lower Cambrian sedimentary sequences in this area was controlled mainly by river systems similar to modern large rivers (catchment area >100 000 km2) and rivers draining sedimentary rocks (catchment area <100 000 km2). The fine-grained aluminosiliciclastics transported by them was delivered mainly from areas composed of rocks of the platform crystalline basement and, in part, sedimentary rocks. The distribution of data points of Vendian–Lower Cambrian mudstones on the (La/Yb)N–Eu/Eu* and (La/Yb)N–Th diagrams with fields of the pelitic and silty–pelitic sediments at the mouths of modern different-category rivers shows that mafic rocks of the Volyn–Brest large igneous province, apparently, were not suppliers of the fine-grained aluminosiliciclastics in the indicated time intervals.

摘要 根据与东欧地台西部(白俄罗斯和沃伦,部分为立陶宛)沃伦群、瓦尔代群和波罗的海群细粒碎屑岩有关的岩石地球化学数据,重建了将细粒铝硅酸盐碎屑岩运往汇水区的河流类别。结论是,该地区文迪纪和下寒武纪沉积序列的形成主要受控于类似于现代大河(集水面积达 100,000 平方公里)的河流系统和排泄沉积岩的河流(集水面积达 100,000 平方公里)。这些河流输送的细粒铝硅酸盐岩主要来自由地台结晶基底岩石和部分沉积岩组成的地区。文登-下寒武统泥岩在(La/Yb)N-Eu/Eu*和(La/Yb)N-Th 图上的数据点分布,以及现代不同类别河流河口的绿泥石和淤泥质绿泥石沉积物区域的分布情况表明,沃伦-布列斯特大型火成岩区的黑云母岩显然不是上述时间段内细粒铝硅酸盐岩的供应者。
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引用次数: 0
Lithological Features of the Uryuk Formation in the Vendian Tolparovo Section (Southern Urals) 南乌拉尔地区托尔帕罗沃段文地宙乌留克地层的岩性特征
IF 0.7 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2024-03-02 DOI: 10.1134/S0024490223700372
V. M. Gorozhanin, S. V. Michurin, V. F. Yuldashbaeva

New results of the lithological structural–textural observations and petrographic study of rocks of the Uryuk Formation (sandstones and gravelstone-sandstones with the subordinate mudstone interlayers) exposed in the Malyi Tolpar River basin in the Bashkir meganticlinorium. For the first time, a wide development of synsedimentary underwater landslide folds (varying from the first tens of centimeters to the first meters in size) has been established in the Uryuk deposits. The sandstones demonstrate the oblique, wavy, flaser, and horizontal (with paired thin clay lamina) stratification, as well as massive layers. Signs of shallow wave ripples have been established. The rocks are characterized by mechanoglyphs and textures similar to Arumberia banksi, which presumably represent the lithified textures of bacterial mats that existed under shallow-marine environments with sandy–clayey sedimentation. Despite the absence of direct lithological signs of diamictites, the Uryuk deposits likely form a single sedimentary sequence with the underlying Tolparovo–Suirovo marine glacial deposits, in which a shallow-sea sedimentation regime was established by the end of the Uryuk time. It is shown that the presence of ferruginous minerals in the sandstone cement is secondary in nature and is associated with their epigenetic transformations. It is concluded that the red color of rocks of the Uryuk Formation cannot be used for the stratification of its sections and reconstruction of sedimentation conditions in the Uryuk time.

摘要:对出露于巴什基尔大峡谷马利托尔帕河流域的乌留克地层(砂岩和砾岩-砂岩及其下层泥岩夹层)岩石进行的岩性结构-纹理观察和岩石学研究取得了新成果。在乌柳克矿床中首次发现了广泛发育的合成沉积水下滑坡褶皱(大小从最初的几十厘米到最初的几米不等)。砂岩呈现出斜向层理、波浪层理、扇形层理、水平层理(带有成对的薄粘土层)以及块状层理。浅波纹的迹象已经确定。这些岩石具有类似于 Arumberia banksi 的机械纹理和质地,推测其代表了在砂质粘土沉积的浅海环境下存在的细菌垫的岩化质地。尽管没有直接的二迭石岩性迹象,但乌留克沉积物很可能与下层的托尔帕罗沃-绥罗沃海洋冰川沉积物形成了一个单一的沉积序列,其中的浅海沉积体系在乌留克时代末期已经形成。研究表明,砂岩胶结物中铁锈色矿物的存在是次生的,与它们的表生转化有关。结论是,乌留克地层岩石的红色不能用于对其剖面进行分层和重建乌留克时期的沉积条件。
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引用次数: 0
Cretaceous–Eocene Flysch of the Sochi Synclinorium (Western Caucasus): Sources of Clastic Material Based on the Results of U–Th–Pb Isotope Dating of Detrital Zircons 索契 Synclinorium(西高加索)白垩纪-始新世的 Flysch:基于碎屑锆石 U-Th-Pb 同位素测定结果的碎屑材料来源
IF 0.7 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2024-03-02 DOI: 10.1134/S0024490223700384
N. B. Kuznetsov, T. V. Romanyuk, A. V. Shatsillo, I. V. Latysheva, I. V. Fedyukin, A. V. Strashko, A. S. Novikova, E. A. Shcherbinina, A. V. Drazdova, E. I. Makhinya, A. V. Marinin, A. S. Dubenskiy, K. G. Erofeeva, V. S. Sheshukov

The first results of the U–Th–Pb isotope dating of detrital zircons (dZr, N = 130, n = 91) from the middle Danian sandstones (63.9–65.3 Ma) of the Cretaceous–Eocene Novorossiisk–Anapa flysch widely developed in the Sochi synclinorium (southern slope of the Western Caucasus) are presented. The maximum and minimum dZr age is 2973 ± 12 Ma and 318 ± 3 Ma, respectively; weighted average age of the four youngest dZr is ~322 ± 7 Ma. There are no signs of erosion products of the Jurassic magmatites involved in the structure of the Greater Caucasus and Crimean Mountains into the sedimentary basin, where the Novorossiisk–Anapa flysch was formed. The results have revealed a high degree of similarity between the provenance signals of the Danian sandstones from the Novorossiisk–Anapa flysch, some Paleogene–Neogene and Early Quaternary (Early Pleistocene) sandstones of the Western Caucasus and Western Cis-Caucasia, red-colored Upper Permian and Lower Triassic sandstones of the Moscow syneclise, as well as Late Quaternary alluvium at lower reaches of the Don and Volga rivers draining vast expanses of the Russian Plate. These facts suggest: (1) the absence of eroded mountain structures of the Greater Caucasus and Crimea in the middle Danian; (2) the main volume of detrital material composing the Novorossiisk–Anapa flysch was formed due to the recycling of Permian–Triassic and younger sequences of the Russian Plate.

摘要 首次公布了对广泛发育于索契(西高加索南坡)的白垩世-始新世新罗西斯克-安纳帕飞天中段砂岩(63.9-65.3 Ma)中的碎屑锆石(dZr,N = 130,n = 91)进行 U-Th-Pb 同位素测年的结果。最大和最小 dZr 年龄分别为 2973 ± 12 Ma 和 318 ± 3 Ma;四个最年轻 dZr 的加权平均年龄约为 322 ± 7 Ma。大高加索山脉和克里米亚山脉的构造所涉及的侏罗纪岩浆岩的侵蚀产物没有进入沉积盆地的迹象,而新罗西斯克-安纳帕飞沙就是在沉积盆地中形成的。研究结果表明,新罗西斯克-安纳帕岩层中的达尼安砂岩、西高加索和西中高加索地区的一些古新统和第四纪早期(早更新世)砂岩、莫斯科合围区的上二叠统和下三叠统红色砂岩,以及顿河和伏尔加河下游的第四纪晚期冲积层的产地信号具有高度的相似性。这些事实表明:(1) 大丹尼中期没有大高加索和克里米亚的侵蚀山体结构;(2) 构成新罗西斯克-阿纳帕沼泽的主要碎屑物质是由于俄罗斯板块二叠纪-三叠纪和更年轻序列的再循环而形成的。
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引用次数: 0
Paleozoic Reef Formation in the Pechora Syneclise and the Caspian Basin: A Comparative Analysis 佩乔拉群落和里海盆地的古生代岩礁形成:对比分析
IF 0.7 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2024-03-02 DOI: 10.1134/S0024490223700360
V. G. Kuznetsov, L. M. Zhuravleva

In two marginal depressions of the East European Platform (Pechora Syneclise and Caspian Basin), reef structures are widespread, but their stratigraphic intervals are far from similar. The reef formation began in the Caradocian in the Pechorian Ural, in the second half of the Llandoverian in the Pechora Syneclise, reached the maximum in the Frasnian, and gave way to the development of reef mounds in the Famennian. The structures are represented both as asymmetric reefs framing shallow zones at their boundary with the relatively deep paleobasins and as solitary structures within the latter. Reefs of the next global maximums (late Visean–Serpukhovian and Lower Permian) are confined to some places at the boundary with the Ural paleocean and its relict (Cis-Ural foredeep). The Caspian Basin accommodates reefs of all three global maximums of development—both asymmetric reef systems framing the shelf edges and symmetric intra-basin isolated structures. Such difference is due to the different paleogeomorphological type of basins. The Caspian Basin was sharply differentiated in depth throughout the Middle and Late Paleozoic, resulting in the formation of reefs rising above the bottom of these basins. In the Pechora Syneclise, depth differentiation of the basins occurred only in the Late Devonian. The Visean–Serpukhovian and early Permian shallow seas were generally weakly dissected and did not provide conditions for the formation of thick reefs protruding above the seafloor. Such reefs were formed only on the Ural paleocean edge in the Visean–Serpukhovian and on the Cis-Ural foredeep edge in the Permian.

摘要 在东欧地台的两个边缘洼地(佩科拉同步带和里海盆地)中,礁石结构十分普遍,但它们的地层间隔却远不相似。礁石的形成始于佩乔拉乌拉尔卡拉多克纪,佩乔拉群的形成始于兰多瓦纪后半期,在弗拉斯年达到顶峰,并在法门年让位于礁丘的发展。这些结构既表现为在与相对较深的古盆地交界处的浅滩上形成不对称的礁框,也表现为古盆地内的孤立结构。下一个全球最大值(晚维西期-瑟普霍夫期和下二叠统)的礁石仅限于与乌拉尔古海洋及其遗迹(顺乌拉尔前深)交界的一些地方。里海盆地容纳了所有三种全球最大发育程度的礁石--既有构成陆架边缘的非对称礁石系统,也有盆地内对称的孤立结构。这种差异是由于盆地的古地貌类型不同造成的。里海盆地在整个中、晚古生代深度分化明显,导致礁石形成,高出盆地底部。在佩乔拉群,盆地的深度分异只发生在晚泥盆世。维谢安-塞普霍维亚和二叠纪早期的浅海一般分隔较弱,不具备形成凸出海底的厚珊瑚礁的条件。只有在维谢安-塞普霍夫期的乌拉尔古海洋边缘和二叠纪的顺乌拉尔前深边缘才形成了这种珊瑚礁。
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引用次数: 0
Special Aspects of the Application of Lithogeochemical Indicators for Reconstructing the Paleoclimate and Composition of Source Areas in the West Siberian Late Jurassic–Lower Cretaceous Sedimentary Basin 应用岩石地球化学指标重建西西伯利亚晚侏罗世-下白垩世沉积盆地古气候和源区组成的特殊方面
IF 0.8 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-11-14 DOI: 10.1134/S0024490223700311
V. G. Eder, A. G. Zamiralova, P. A. Yan

For Upper Jurassic–Lower Cretaceous rocks of the Bazhenov Formation, a significant positive linear correlation of the content of Th, Hf, Sc, and La with the Al2O3 content was revealed, and their terrigenous genesis was confirmed. It has been determined that the samples, in which the distribution of Sc/Al2O3 and La/Al2O3 values does not satisfy the linear correlation, represent the mixed clayey–siliceous rocks (with P2O5 > 1 wt %) or the substantially pyritized rocks (with the pyrite content exceeding the OM content and C/S ≤ 1), as well as siliceous mudstones (with the SiO2 content > 70 wt %). It is concluded that, in addition to carbonatized rocks, rocks of the above-mentioned types, as well as rocks subjected to the late diagenetic kaolinization, should be excluded before analyzing the geochemical indicators for reconstructing the formation conditions of the Bazhenov Formation. The formation conditions of these rocks were reconstructed based on the analysis of values of several geochemical modules and indicators. Based on the study of CIA and CIW variations, it was confirmed that the Late Jurassic–Early Cretaceous climate in the West Siberian sedimentary basin was warm and semiarid, and it did not change significantly during the entire period under consideration. For rocks of the Bazhenov Formation, several indicators, such as (La/Yb)N and Eu/Eu*, as well as the distribution of trace elements in the Th‒La‒Sc triangular diagram, suggest that rocks of the Bazhenov Formation were deposited in the central and southeastern regions, with the dominant impact of source areas of mafic rocks.

上侏罗统—下白垩统Bazhenov组岩石中Th、Hf、Sc、La含量与Al2O3含量呈显著的线性正相关,证实了其陆源成因。样品中Sc/Al2O3和La/Al2O3值的分布不满足线性相关关系,代表混合粘土-硅质岩石(含P2O5 >1 wt %)或大部分黄铁矿化的岩石(黄铁矿含量超过OM含量且C/S≤1),以及硅质泥岩(SiO2含量>70% wt %)。在分析地球化学指标重建巴热诺夫组形成条件时,除碳酸化岩石外,应排除上述类型的岩石以及晚成岩高岭土化作用的岩石。通过对多个地球化学模块和指标值的分析,重建了这些岩石的形成条件。通过对CIA和CIW变化的研究,证实了西西伯利亚沉积盆地晚侏罗世-早白垩世气候为温暖半干旱气候,且在整个研究时期没有明显变化。(La/Yb)N和Eu/Eu*等指标以及Th-La-Sc三角图中微量元素的分布表明,巴济诺夫组岩石主要沉积在中部和东南部地区,主要受基性岩源区的影响。
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引用次数: 0
Sorption Properties of Cobalt-Bearing Ferromanganese Crusts on the Kocebu Guyot of the Magellan Seamounts Relative to Rare-Earth Metal Cations 含钴锰铁结壳在麦哲伦海山高部岩上对稀土金属阳离子的吸附特性
IF 0.8 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-11-14 DOI: 10.1134/S0024490223700347
G. V. Novikov, N. V. Lobus, O. Y. Bogdanova

The results of experimental studies of the sorption properties of ferromanganese crusts on the Kocebu Guyot relative to rare-earth metal (REM) cations are presented. It is established that the crusts are a natural, highly selective sorbent of REM cations. The REM cations are adsorbed on ore minerals (Fe-vernadite, vernadite, Mn-feroxyhyte, and goethite). The crusts are characterized by a high exchange capacity (1.67‒3.28 mg-equiv/g), which increases in the series: Lu < Gd < Dy < La, Sm < Nd < Y < Eu ( ll ) Ce. The REM cations are adsorbed by the ion-exchange equivalent mechanism—in the case of Ce3+ cations, according to the superequivalent mechanism with respect to cations of the exchange complex of ore minerals—Na+, K+, Ca2+, Mg2+, Mn2+, and Ni2+, which contribute 95–98% to the total capacity of minerals.

本文介绍了铁锰结壳在高釜土上对稀土离子吸附性能的实验研究结果。研究表明,这些结壳是一种天然的、高选择性的REM阳离子吸附剂。REM阳离子吸附在矿石矿物(铁-vernadite, vernadite, mn - feroxyhyite和针铁矿)上。地壳具有较高的交换容量(1.67 ~ 3.28 mg-equiv/g),交换容量随序列的增大而增大:d &lt;Dy &lt;La, Sm &lt;Nd &lt;Y &lt;Eu ( ll ) Ce。REM阳离子通过离子交换等效机制被吸附,在Ce3+阳离子的情况下,根据矿物交换配合物阳离子的超等效机制- na +, K+, Ca2+, Mg2+, Mn2+和Ni2+,贡献95-98% to the total capacity of minerals.
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引用次数: 0
Multi-Stage Tectonothermal Events in the Nageng Mining Area, East Kunlun, China: Evidence from In Situ U–Pb Dating of Apatite and Zircon 东昆仑那庚矿区多期构造热事件:磷灰石和锆石原位U-Pb定年证据
IF 0.8 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-11-14 DOI: 10.1134/S002449022370027X
Chen Jing

The Nagengkancherer (“Nageng”) silver deposit is the only independent silver mine in Qinghai Province, China. Here, the results of LA–ICP–MS U–Pb dating of apatite and zircon in quartz veins in this area are reported for the first time. The apatite is homogeneous and bright, with characteristics typical of unaltered magmatic apatite that has been unaffected by fluid. The zircons display oscillatory zonation typical of a magmatic origin. Apatite and zircon ages of the Paleoproterozoic Jinshuikou Group are older than those of the Triassic Erashan Formation, with apatite lower-intercept ages of 409.0 ± 3.7 and 376.2 ± 5.6 Ma, respectively, consistent with 207Pb-corrected ages and representing the two formation ages of apatite minerals. The zircon weighted-mean 206Pb/238U age is 425.2 ± 1.8 Ma, with ages of 425–408 Ma being consistent those of late Silurian outcrops on the periphery of the mining area. This indicates the occurrence of a major tectonothermal event in the late Silurian–Early Devonian, revealing the existence of concealed rock at depth in the mining area and providing new information concerning the geological characteristics of the mining area. The age of 376 Ma is reported here for the first time and provides new constraints on the regional tectonic evolution. One sample from the Erashan Formation contained magmatic zircons with a U–Pb age of 220 ± 0.62 Ma, which represents the age of the country rocks (Erashan rhyolite) captured during the ascent of ore-forming hydrothermal fluids.

那根坎彻尔(“那根”)银矿是中国青海省唯一的独立银矿。本文首次报道了该地区石英脉中磷灰石和锆石的LA-ICP-MS U-Pb定年结果。磷灰石均匀明亮,具有未受流体影响的未蚀变岩浆岩磷灰石的典型特征。锆石显示岩浆成因的振荡分带。古元古代金水口群磷灰石和锆石年龄均高于三叠系腊山组,磷灰石下截年龄分别为409.0±3.7 Ma和376.2±5.6 Ma,与207pb校正年龄一致,代表了磷灰石矿物的两种形成年龄。锆石206Pb/238U加权平均年龄为425.2±1.8 Ma, 425 ~ 408 Ma与矿区外围晚志留世露头年龄一致。这表明晚志留世—早泥盆世曾发生过一次重大构造热事件,揭示了矿区深部隐伏岩的存在,为矿区地质特征提供了新的信息。本文首次报道了376 Ma的年龄,为区域构造演化提供了新的约束条件。峨山组岩浆岩锆石U-Pb年龄为220±0.62 Ma,代表了成矿热液上升过程中捕获的围岩(峨山流纹岩)的年龄。
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引用次数: 0
Grain Size Composition of Neopleistocene Basal Moraines in the Northeasternmost Area of the Russian Plain 俄罗斯平原最东北部新更新世基底冰碛的粒度组成
IF 0.8 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-11-14 DOI: 10.1134/S002449022370030X
L. N. Andreicheva

Generalization of the grain size analyses of the basal Neopleistocene moraines from the sections of coastal outcrops and boreholes in the vast European Subarctic region of Russia and in more southern areas of the Timan–Pechora–Vychegda region showed that the moraines are typical mixed, almost unsorted rocks with similar contents of the gravel–sand, silt, and clay fractions, serving as one of the arguments in favor of their glacial genesis. Their grain size composition is related to the peculiarities of rocks in the glacier bed. It is formed during the crushing, abrasion, and mixing of the glacier-rafted, assimilated, and transported material during its transportation and deposition, which determines variability of the grain size composition of moraines. Consequently, the grain size composition of moraines in combination with other lithological data reflects the pathway and dynamics of the glacier movement.

从俄罗斯广阔的欧洲亚北极地区和蒂曼-佩霍拉-维切格达地区更南部地区的沿海露头剖面和钻孔中对基底新更新世冰碛石的粒度分析的概括表明,这些冰碛石是典型的混合岩石,几乎没有分选,砾石-砂、淤泥和粘土组分的含量相似,这是支持其冰川成因的论据之一。它们的粒度组成与冰川床中岩石的特性有关。它是在冰川漂流、同化和搬运的物质在搬运和沉积过程中破碎、磨蚀和混合形成的,这决定了冰碛石粒度组成的可变性。因此,冰碛石粒度组成结合其他岩性资料反映了冰川运动的路径和动力学。
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引用次数: 0
Model of the Gold-Bearing Placer Formation in Platform Areas (Eastern Siberian Platform) 台地区(东西伯利亚台地)含金砂矿形成模式
IF 0.8 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-11-14 DOI: 10.1134/S0024490223700232
Z. S. Nikiforova, Y. A. Kalinin, V. A. Naumov, A. V. Lalomov

A model of the gold-bearing placer formation in platform areas is proposed for the first time. Placers on the platforms are formed mainly due to the Precambrian ore sources spatially confined to the basement outcrops, and, locally, Mesozoic sources formed during the tectonomagmatic activation in the paleorift and deep fault zones. Placers related to the Precambrian sources are characterized by the presence of fine and thin gold (size 0.1‒0.25 mm) and, as a rule, are not of commercial interest. They make up alluvial bar and coastal-marine allochthonous placers. They are considered as complex (mainly rare metal–titanium) placers, where gold occurs as associated component). Placers related to sources of the Mesozoic ore formation stage are assigned to the class of small and medium reserves (gold size ranging from the dust-size to 0.2‒0.25 mm or more) and are usually mined by prospectors' teams. Placers on the platforms do not make up sheet deposits, since they are formed mainly due to sources that do not generate placers. The presence of such placers indicates the proximity of ore occurrence, whose type and location can be determined based on the study of mineralogical-geochemical features of the placer gold.

首次提出了台地地区含金砂矿形成模式。台地砂主要由空间上局限于基底露头的前寒武纪矿源形成,局部由古裂谷和深断裂带构造岩浆活动形成的中生代矿源形成。与前寒武纪来源有关的砂矿的特征是存在细而薄的金(尺寸为0.1-0.25 mm),通常没有商业价值。它们构成了冲积沙洲和海岸-海洋异质砂。它们被认为是复杂的(主要是稀有金属钛)砂矿,其中金作为伴生成分出现。与中生代成矿阶段来源有关的砂矿被划分为中小型储量(金粒度从粉尘到0.2-0.25毫米或更大),通常由探矿队开采。平台上的砂矿不构成片状矿床,因为它们主要是由不产生砂矿的来源形成的。这类砂矿的存在表明矿床的赋存距离较近,通过对砂金矿物学地球化学特征的研究,可以确定矿床的类型和位置。
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引用次数: 0
Postsedimentary Transformations of Silurian Carbonate Rocks on the Central Part of the Chernyshev Ridge (Timan–Pechora Province) 车尔尼雪夫岭中部志留系碳酸盐岩的沉积后转化
IF 0.8 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2023-11-14 DOI: 10.1134/S0024490223700293
I. I. Danshikova, T. V. Maydl

The article presents the results of studies of postsedimentary processes in Silurian carbonate rocks of the central part of the Chernyshev Ridge. A complex combination of secondary transformations in carbonate reservoir is shown. The sedimentary sequences show manifestations of regional and superimposed lithogenesis. In addition to stagewise catagenetic changes, the sediments were also subjected to regressive infiltration catagenesis (epigenesis), which was accompanied by leaching and dolomitization of limestone. All this significantly affected the filtration–capacitive properties. The obtained data can contribute to the identification of new objects for exploration drilling and optimization of exploration works in complex regions.

本文介绍了车尔尼雪夫岭中部志留系碳酸盐岩沉积后作用的研究结果。碳酸盐岩储层表现出复杂的次生转化组合。沉积层序表现为区域性、叠合性成岩作用。沉积物除经历阶段性变质作用外,还经历了退行性入渗变质作用(后成作用),并伴有灰岩的淋溶和白云化作用。这些都显著影响了过滤电容性能。获得的数据有助于识别新的勘探钻孔目标和优化复杂区域的勘探工作。
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Lithology and Mineral Resources
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