Готові списки джерел за темами / Tectonic provenance

Добірка наукової літератури з теми "Tectonic provenance"

Автор: Grafiati
Опубліковано: 10 грудня 2022
Оновлено: 28 січня 2023

Оформте джерело за APA, MLA, Chicago, Harvard та іншими стилями

Оберіть тип джерела:

Зміст

Ознайомтеся зі списками актуальних статей, книг, дисертацій, тез та інших наукових джерел на тему "Tectonic provenance".

Біля кожної праці в переліку літератури доступна кнопка «Додати до бібліографії». Скористайтеся нею – і ми автоматично оформимо бібліографічне посилання на обрану працю в потрібному вам стилі цитування: APA, MLA, «Гарвард», «Чикаго», «Ванкувер» тощо.

Також ви можете завантажити повний текст наукової публікації у форматі «.pdf» та прочитати онлайн анотацію до роботи, якщо відповідні параметри наявні в метаданих.

Статті в журналах з теми "Tectonic provenance"

1

Chen, Xingyu, Zhijie Zhang, Xuanjun Yuan, Li Wan, Chuanmin Zhou, Yinhe Liu, and Dawei Cheng. "The Evolution of Permian Source-to-Sink Systems and Tectonics Implications in the NW Junggar Basin, China: Evidence from Detrital Zircon Geochronology." Minerals 12, no. 9 (September 15, 2022): 1169. http://dx.doi.org/10.3390/min12091169.

Повний текст джерела
Анотація:
The basin type of the Junggar Basin changed during the Permian, but the time constraint of the tectonic evolution remains unclear. Besides, the fan deltas developed in the Permian in the Mahu Sag in the northwestern of the oil-rich basin. However, the provenances of the sedimentary systems remain unclear. Based on petrology and detrital zircon U-Pb ages, this study investigates the source-to-sink systems evolution and tectonics implications. Abundant lithic clasts in sandstones with low compositional and textural maturity imply proximal sources. The dating results showed a dominant peak (310–330 Ma) and a secondary peak (400–440 Ma) in the northern Mahu Sag, only one peak at 295–325 Ma in the central Mahu Sag, several peaks at 270–350 Ma in the southern Mahu Sag, and multiple peaks at 370–450 Ma in the Zhongguai Uplift. Thus, the north-western Junggar Basin was divided into four major source-to-sink systems, with adjacent central West Junggar as the main provenance and northern and southern West Junggar as the secondary provenance. The proportion of sediment supply from the southern and northern West Junggar is higher during the Middle-Late Permian. It suggests that the source-to-sink systems show inheritance and evolve from a single provenance into a complex provenance, indicating the uplift of West Junggar. The tectonic inversion may occur early in the Middle Permian and the response to tectonic activity is stronger in the southern West Junggar than in the northern West Junggar.
Стилі APA, Harvard, Vancouver, ISO та ін.
2

Zhang, Yue Qiao, Wei Hou, and Fang Zhang. "The Provenance Tectonic Background Analysis of the Upper Jurassic Mohe Basin in Northeast China." Advanced Materials Research 734-737 (August 2013): 476–79. http://dx.doi.org/10.4028/www.scientific.net/amr.734-737.476.

Повний текст джерела
Анотація:
The provenance tectonic background of Late Jurassic Mohe Basin was researched through the geochemical composition of sandstone. The Late Jurassic Mohe Basin is characterized by multiple provenances. One provenance is the active continental margin, and another is the island arc. Comparing with the regional lithology, the active continental margin may be from the Mongolia-Okhotsk orogenic belt, and the island arc may be from the northern of the Da Hingan Mountains. The characteristics are concerned with its geotectonic position.
Стилі APA, Harvard, Vancouver, ISO та ін.
3

Baiyegunhi, Temitope Love, Kuiwu Liu, Oswald Gwavava, Christopher Baiyegunhi, and Maropene Rapholo. "Geochemistry of the mudrocks and sandstones from the Bredasdorp Basin, offshore South Africa: Implications for tectonic provenance and paleoweathering." Open Geosciences 13, no. 1 (January 1, 2021): 1187–225. http://dx.doi.org/10.1515/geo-2020-0260.

Повний текст джерела
Анотація:
Abstract An inorganic geochemical investigation of mudrocks and sandstone from the southern Bredasdorp Basin, off the south coast of South Africa was carried out to unravel the provenance, paleoweathering, and tectonic setting of the basin. Seventy-seven representative samples from exploration wells E-AH1, E-AJ1, E-BA1, E-BB1, and E-D3 underwent geochemical analysis involving major and trace elements. The major oxide compositions show that the sandstones could be classified as sub-arkose and sub-lithic arenite. The provenance discrimination diagrams based on major oxide geochemistry revealed that the sandstones are mainly of quartzose sedimentary provenance, while the mudrocks are of quartzose sedimentary and intermediate igneous provenances. The discrimination diagrams indicate that the Bredasdorp sediments were mostly derived from a cratonic interior or recycled orogen. The bivariate plots of TiO2 versus Ni, TiO2 against Zr, and La/Th versus Hf as well as the ternary diagrams of V–Ni–Th∗10 suggest that the mudrocks and sandstones were derived from felsic igneous rocks. The tectonic setting discrimination diagrams support passive-active continental margin setting of the provenance. Also, the closely similar compositions of the analysed samples and recent sedimentary rocks of the East African Rift System perhaps suggest a rifted basin tectonic setting for the Bredasdorp Basin. Chemical index of alteration (CIA) indices observed in the sandstones suggest that their source area underwent low to moderate degree of chemical weathering. However, the mudrocks have high CIA indices suggesting that the source area underwent more intense chemical weathering, possibly due to climatic and/or tectonic variations.
Стилі APA, Harvard, Vancouver, ISO та ін.
4

Baiyegunhi, Temitope Love, Kuiwu Liu, Oswald Gwavava, and Christopher Baiyegunhi. "Petrography and Tectonic Provenance of the Cretaceous Sandstones of the Bredasdorp Basin, off the South Coast of South Africa: Evidence from Framework Grain Modes." Geosciences 10, no. 9 (August 28, 2020): 340. http://dx.doi.org/10.3390/geosciences10090340.

Повний текст джерела
Анотація:
The Cretaceous sandstones of the Bredasdorp Basin were investigated to recognize their composition, provenance, and tectonic setting. Ninety-two samples of sandstones from exploration wells E-AH1, E-AJ1, E-BA1, E-BB1, and E-D3 were investigated using both petrographic and X-ray diffraction (XRD) methods. Petrographic studies based on quantitative investigation of the detrital framework grain shows that the Bredasdorp sandstones chiefly consist of quartz (52.2–68.0%), feldspar (10.0–18.0%), and lithic fragments (5.0–10.2%). These sandstones are mostly fine grained, moderately well-sorted, and subrounded to rounded. The modal composition data shows that the sandstones could be classified as subarkosic arenite and lithic arkose. Such a composition of the sandstones perhaps indicates the interplay of pulses of fast uplift of the source area and rapid subsidence of the Bredasdorp Basin, with subsequent periods of calmness within the transgressive-regressive sequence in a rift tectonic regime. The provenance ternary diagrams revealed that the sandstones are mainly of continental block provenances (stable shields and basement uplifted areas) and complemented by recycled sands from an associated platform. The tectonic provenance studies of Bredasdorp Basin revealed that the sandstones are typically rift sandstones and have undergone long-distance transport from the source area along the rift. In the regional context of the evolution of the Bredasdorp Basin, the results presented in this study inferred that the basin developed on a rift passive setting (trailing edge) of the stable continental margins.
Стилі APA, Harvard, Vancouver, ISO та ін.
5

McCarthy, Odhrán, Brenton Fairey, Patrick Meere, David Chew, Aidan Kerrison, David Wray, Mandy Hofmann, et al. "The provenance of Middle Jurassic to Cretaceous sediments in the Irish and Celtic Sea Basins: tectonic and environmental controls on sediment sourcing." Journal of the Geological Society 178, no. 5 (March 23, 2021): jgs2020–247. http://dx.doi.org/10.1144/jgs2020-247.

Повний текст джерела
Анотація:
The Jurassic and Cretaceous sedimentary infill of the Irish and Celtic Sea Basins is intimately associated with the breakup of the supercontinent Pangea, and the opening of the Atlantic margin. Previous basin studies have constrained tectonism, basin uplift and sediment composition, but sediment provenance and routing have not received detailed consideration. Current hypotheses for basin infill suggest localized sediment sourcing throughout the Jurassic and Cretaceous, despite a dynamic tectonic and palaeoenvironmental history spanning more than 100 million years. We present detrital zircon, white mica and apatite geochronology alongside heavy mineral data from five basins. Findings reveal that basin infill derived predominantly from distal sources with lesser periods of local sourcing. We deduce that tectonically induced marine transgression and regression events had a first-order control on distal v. proximal sedimentary sourcing. Additionally, tectonism which uplifted the Fastnet Basin region during the Middle–Late Jurassic recycled basin sediments into the connected Celtic and Irish Sea Basins. Detrital geochronology and heavy mineral evidence support three distinct provenance switches throughout the Jurassic and Cretaceous in these basins. Overall an integrated multi-proxy provenance approach provides novel insights to tectonic and environmental controls on basin infill as demonstrated in the Irish and Celtic Sea Basins.Supplementary material: Tables S1–S6 are available at https://doi.org/10.6084/m9.figshare.c.5343657
Стилі APA, Harvard, Vancouver, ISO та ін.
6

Xu, Tao, Ling Feng, Wen Yin, Jinpeng Wei, Yarong Wang, and Xianli Zou. "Element Geochemical Characteristics and Provenance Conditions of the 1st Member of Jurassic Zhongjiangou Formation in Wudun Sag, Dunhuang Basin." Applied Sciences 12, no. 9 (April 20, 2022): 4110. http://dx.doi.org/10.3390/app12094110.

Повний текст джерела
Анотація:
In order to clarify the provenance of the 1st member of the Zhongjiangou formation in Wudun sag, Dunhuang basin, the structural attributes, weathering and sedimentary characteristics of the provenance area were analyzed by means of element geochemistry, so as to determine the differences of sediment sources in different well areas. The results show that the higher the Al2O3 and K2O contents, the higher the enrichment of large ion lithophile elements and high field strength elements, while the iron and magnesium elements are relatively deficient, and there are characteristics of medium degree differentiation of light and heavy rare earth elements in Well XC1 and Well D2. The lower the Al2O3 content and the higher the SiO2 content, a loss of large ion lithophile elements and high field strength elements are observed, while the ferrophilic magnesium elements show serious loss, as shown in the characteristics of the high degree of differentiation of light and heavy rare earth elements in Well D1. In the UCC-normalized element spidergrams, the trend of Well XC1 and Well D2 is similar, which is different from that of well D1, indicating that the sediments of Well XC1 and Well D2 come from the same provenance area, while the sediment of Well D1 comes from a different provenance area. The provenance area of Well XC1 and Well D2 shows strong tectonic activity and strong weathering, while the provenance area of well D1 exhibits relatively weak tectonic activity and weathering. Combined with previous research results, Wudun sag is mainly characterized by a faulted lacustrine basin controlled by the southern boundary fault in the Jurassic layer. Therefore, the sediments of Well XC1 and Well D2 mainly come from the southern Sanweishan uplift provenance area, with strong tectonic activity; the sediments of Well D1 mainly come from the northern Beishan provenance area, with relatively weak tectonic activity.
Стилі APA, Harvard, Vancouver, ISO та ін.
7

Li, Yalong, Wei Yue, Xun Yu, Xiangtong Huang, Zongquan Yao, Jiaze Song, Xin Shan, Xinghe Yu, and Shouye Yang. "Tectonic Evolution of the West Bogeda: Evidences from Zircon U-Pb Geochronology and Geochemistry Proxies, NW China." Minerals 10, no. 4 (April 10, 2020): 341. http://dx.doi.org/10.3390/min10040341.

Повний текст джерела
Анотація:
The Bogeda Shan (Mountain) is in southern part of the Central Asian Orogenic Belt (CAOB) and well preserved Paleozoic stratigraphy, making it an ideal region to study the tectonic evolution of the CAOB. However, there is a long-standing debate on the tectonic setting and onset uplift of the Bogeda Shan. In this study, we report detrital zircon U-Pb geochronology and whole-rock geochemistry of the Permian sandstone samples, to decipher the provenance and tectonic evolution of the West Bogeda Shan. The Lower-Middle Permian sandstone is characterized by a dominant zircon peak age at 300–400 Ma, similar to the Carboniferous samples, suggesting their provenance inheritance and from North Tian Shan (NTS) and Yili-Central Tian Shan (YCTS). While the zircon record of the Upper Permian sandstone is characterized by two major age peaks at ca. 335 Ma and ca. 455 Ma, indicating the change of provenance after the Middle Permian and indicating the uplift of Bogeda Shan. The initial uplift of Bogeda Shan was also demonstrated by structural deformations and unconformity occurring at the end of Middle Permian. The bulk elemental geochemistry of sedimentary rocks in the West Bogeda Shan suggests the Lower-Middle Permian is mostly greywacke with mafic source dominance, and tectonic setting changed from the continental rift in the Early Permian to post rift in the Middle Permian. The Upper Permian mainly consists of litharenite and sublitharenite with mafic-intermediate provenances formed in continental island arcs. The combined evidences suggest the initial uplift of the Bogeda Shan occurred in the Late Permian, and three stages of mountain building include the continental rift, post-rift extensional depression, and continental arc from the Early, Middle, to Late Permian, respectively.
Стилі APA, Harvard, Vancouver, ISO та ін.
8

van de Kamp, Peter C., and Bernard Elgey Leake. "Petrography and geochemistry of feldspathic and mafic sediments of the northeastern Pacific margin." Transactions of the Royal Society of Edinburgh: Earth Sciences 76, no. 4 (1985): 411–49. http://dx.doi.org/10.1017/s0263593300010646.

Повний текст джерела
Анотація:
ABSTRACTThis study attempts to ascertain whether the differing provenance sources and plate tectonic settings of deposition of clastic sediments and rocks can be identified by chemical means, thus opening the increased use of these rocks and their metamorphosed derivatives in plate tectonic modelling. Mineralogically immature feldspathic and mafic sands, muds, sandstones and shales from Mesozoic, Cenozoic and Holocene clastic deposits in California, Oregon, Alaska and Colorado have been both modally and chemically analysed providing a valuable data base (217 samples; 216 samples chemically analysed, many for 28 elements).There is significant upward chemical variation in the Great Valley sequence of California which mimics previously described petrographic variation and in turn reflects provenance changes with igneous episodes and erosional stripping of the Sierra Nevada in late Mesozoic time. Differing sandstone petrofacies result in varying chemical signatures and while the provenances of monomict sediments are easiest to identify, polymict sources involving granitoid or ophiolitic material can often be identified by potassium feldspar or Cr contents. The distinction of K which is derived from detrital potassium feldspar from K derived from detrital illite, micas or other sheet minerals, is best made by a Niggli al–alk plot against k. Mafic sandstones derived from mafic volcanic or plutonic rocks preserve essentially mafic igneous chemistry and could be possible parent sources of some amphibolites which grade into metasediments. The lithified erosion products of the Sierra Nevada calc-alkaline igneous rocks have higher Niggli al–alk and higher average Niggli si at any given mg value than the fresh igneous rocks enabling meta-arkoses to be distinguished from meta-igneous rocks.Applying previously published chemical criteria gives the actual plate tectonic setting of deposition of most of the sandstones studied. This suggests that the chemical composition of sandstones can yield much more information about the provenance and plate tectonic setting than hitherto recognised.
Стилі APA, Harvard, Vancouver, ISO та ін.
9

Cui, Liwei, Nan Peng, Yongqing Liu, Dawei Qiao, and Yanxue Liu. "Detrital Zircon Geochronology and Tectonic Evolution Implication of the Middle Jurassic Zhiluo Formation, Southern Ordos Basin, China." Minerals 13, no. 1 (December 27, 2022): 45. http://dx.doi.org/10.3390/min13010045.

Повний текст джерела
Анотація:
The Ordos Basin’s southern part is a composite zone made up of numerous continental blocks and has long been influenced by surrounding tectonism. However, only a few studies have investigated the existence of southern provenance supply and the basin’s southern boundary in the Middle Jurassic Zhiluo Formation. Based on sandstone detrital zircon U-Pb dating and zircon rare earth element analyses, net-sand ratio maps, paleocurrent direction and the field outcrop survey, this study establishes the source area and boundary of the Zhiluo Formation in the southern basin, and discusses the tectonic events. The study shows that the four main age peaks in the detrital spectra occurs at 2283 Ma, 1788 Ma, 432.5 Ma and 218.7 Ma, with a few of the zircons dated at 794.5–1235.2 Ma. The North Qilian orogenic belt (N-QLOB), the western part of the North Qinling orogenic belt (NQOB), and the southern margin of the North China Block (SNCB) contributed to the provenance. According to an integrated analysis of the provenance and tectonic background of continental blocks in the basin’s southern margin, the boundary of the basin in the depositional period of the Zhiluo Formation should reach the N-QLOB in the southwest, the NQOB in the south, and the Sanmenxia–Lushan fault belt in the southeast. On the basis of the aforementioned findings, the tectonic evolution of the continental blocks at the southern periphery of the Ordos Basin was restored.
Стилі APA, Harvard, Vancouver, ISO та ін.
10

Itiowe, K., F. A. Lucas, and E. O. Avwenagha. "Geochemical Analysis of Sediments from Sahaiawei-1 Well of the Northern Delta Depobelt in the Niger Delta Basin, Nigeria." Journal of Scientific Research 13, no. 1 (January 1, 2021): 125–35. http://dx.doi.org/10.3329/jsr.v13i1.48455.

Повний текст джерела
Анотація:
Geochemical analysis of sediments from Sahaiawei-1 Well of the Northern Delta Depobelt in the Niger Delta Basin was carried out to classify the sediments, determine the provenance, tectonic setting and depositional environment. Twenty (20) ditch cutting samples between 1500 and 10730 ft. were subjected to X-ray fluorescence analysis to determine the elemental composition. The result for the classification of the sediments shows that the sediments were classified as Fe-shale and Fe-sand. The discriminant function diagrams for provenance signature and tectonic setting show that the sediments were plotted within the quartzose sedimentary provenance and passive continental margin tectonic setting fields respectively. The depositional environment using inorganic geochemistry shows that the sediments were deposited with in the continental, transitional and marine environments. This research has provided up to date information on the geochemistry of the Northern Delta Depobelt which would help in hydrocarbon exploration in the area.
Стилі APA, Harvard, Vancouver, ISO та ін.
Більше джерел

Дисертації з теми "Tectonic provenance"

1

McArthur, Kelsey L. "Tectonic reconstruction and sediment provenance of a far-traveled nappe, west-central Norway." Laramie, Wyo. : University of Wyoming, 2007. http://proquest.umi.com/pqdweb?did=1475187641&sid=15&Fmt=2&clientId=18949&RQT=309&VName=PQD.

Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
2

Sobczak, Katarzyna. "Investigating far-field tectonic events as drivers of provenance change in sedimentary basins." Thesis, Queensland University of Technology, 2019. https://eprints.qut.edu.au/132493/1/Katarzyna_Sobczak_Thesis.pdf.

Повний текст джерела
Анотація:
This thesis greatly enhanced our understanding of the continental-scale links between sedimentary basins and far-field tectonic processes. A novel, multi-method approach was used to reveal a previously unknown, major mountain building event in southwest Queensland that fundamentally altered the history of the Drummond Basin in central Queensland. An unusually large river system was identified, which transported the gravel and sand across the basin from a distant source region. This thesis has provided new insights into the mid-Paleozoic geological history of the Australian continent, established new approaches to tracing the origin of sediment and resolving the complex histories of sedimentary basins.
Стилі APA, Harvard, Vancouver, ISO та ін.
3

Pettersson, Carl Henrik. "The tectonic evolution of northwest Svalbard." Doctoral thesis, Stockholms universitet, Institutionen för geologiska vetenskaper, 2010. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-39364.

Повний текст джерела
Анотація:
Svalbard represents the uplifted and exhumed northwest corner of the Barents Sea Shelf. Pre-Carboniferous rocks of Svalbard are divided into the Eastern, Northwestern and Southwestern Terranes, were amalgamated during the Caledonian Orogen and are separated by north-south-trending strike-slip faults. Even though our knowledge of Svalbard’s pre-Carboniferous history has increased dramatically during the last two decades, a major issue remains: Where did the different tectonostratigraphic terranes of Svalbard originate? The answer to this question has profound significance for the entire eastern Laurentian margin, which spans two supercontinent cycles, from the amalgamation and breakup of Rodinia to the amalgamation of Pangea. This thesis constrains the tectonothermal evolution of Svalbard’s Northwestern Terrane (NWT) using ion microprobe and LA-ICP-MS U-Pb zircon geochronology and electron microprobe thermobarometry on metasediments, clastic rocks and granitoids. Detrital zircon age populations of metasediments from the NWT suggests that they (e.g. the Krossfjorden Group) were deposited at c. 1000 Ma in a remnant ocean basin setting outboard the Eastern Grenville Province and were subsequently deformed and intruded by Late Grenvillian granitoids during the final suturing of Rodinia. Thus, a northern branch of the Grenvillian/Sveconorwegian orogeny is not present. This older history of the NWT is extensively overprinted by Late Caledonian deformation and metamorphism, with peak metamorphic conditions of 850 °C at >6 kbars, and subsequent migmatization of the Krossfjorden Group at c. 420 Ma. Based on these data, together with the detrital zircon age population from overlying Late Silurian-Early Devonian clastic rocks, a unifying model is proposed involving fragments from the Grampian orogen and Avalonian crust originally accreted to the Laurentian margin, subsequently transported northwards along sinistral strike-slip faults during Scandian deformation.
At the time of the doctoral defense, the following papers were unpublished and had a status as follows: Paper 2: Submitted. Paper 4: In press.
Стилі APA, Harvard, Vancouver, ISO та ін.
4

Zhang, Xiaojing. "Tectonic Evolution of Taimyr in the Late Paleozoic to Mesozoic from Provenance and Thermochronological Evidence." Doctoral thesis, Stockholms universitet, Institutionen för geologiska vetenskaper, 2015. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-119046.

Повний текст джерела
Анотація:
The Taimyr Peninsula is a key element in the circum-Arctic region and represents thenorthern margin of the Siberian Craton. The Taimyr Peninsula is a late Paleozoic fold andthrust belt and preserves late Paleozoic through Mesozoic siliciclastic sedimentarysuccessions and providing an ideal location to investigate the Paleozoic to Mesozoictectonic evolution associated with the Uralian orogeny, the Siberian Trap magmatism andopening of Amerasia Basin within a circum-Arctic framework. Multiple methods areadopted, including petrography, heavy mineral analysis and detrital zircon U-Pbgeochronology for provenance investigation, apatite fission track dating for revealingthermal history and balanced cross section for understanding the deformation style ofTaimyr.The results of this thesis indicate that the Late Carboniferous to Permian sediments ofsouthern Taimyr were deposited in a pro-foreland basin of the Uralian orogen during theUralian orogeny. In the Triassic, the siliciclastic deposits still show a strong Uraliansignature but the initiation of Siberian Trap-related input begins to be significant. Erosionof the Uralian orogen has reached a deep metamorphic level. By Late Jurassic andCretaceous time, the deposition setting of southern Taimyr is an intracratonic basin.Erosion and input from Uralian sources waned while greater input from SiberianTrap-related rocks of the Taimyr region dominated. The Taimyr Peninsula underwent atleast three cooling and uplifting episodes: 280 Ma, 250 Ma and 220 Ma, corresponding tothe Uralian orogeny, the Siberian Traps and the late Triassic transpression.

At the time of the doctoral defense, the following papers were unpublished and had a status as follows: Paper 1: Manuscript. Paper 2: In press. Paper 3: Manuscript. Paper 4: Manuscript.

Стилі APA, Harvard, Vancouver, ISO та ін.
5

Dayong, Vivian Anak. "Geochemistry and Mineralogy of Clastic Sediments of Tukau Formation: Implications on Provenance and Tectonic Setting." Thesis, Curtin University, 2018. http://hdl.handle.net/20.500.11937/75247.

Повний текст джерела
Анотація:
A study is proposed on the clastic sedimentary rocks of the Tukau Formation in the North-West Borneo using combined methods (i.e. geochemistry and petrography) to infer the provenance, tectonic setting and paleoweathering. Generally, Tukau sandstones are classified into quartz arenites , sublitharenites, litharenites, wacke and shale. Source rock is derived from the sedimentary to meta-sedimentary rocks dominated source with minor contribution from granitoids and ultramafic rocks. Tectonically, the Tukau Formation sedimentary rocks were deposited in a passive margin with minor extent towards active margin boundary.
Стилі APA, Harvard, Vancouver, ISO та ін.
6

Peterson, John Aaron. "Geochemical Provenance of Clastic Sedimentary Rocks in the Western Cordillera: Utah, Colorado, Wyoming, and Oregon." DigitalCommons@USU, 2009. https://digitalcommons.usu.edu/etd/439.

Повний текст джерела
Анотація:
Sedimentary rocks are an important source of information about previous orogenic conditions and the composition of which may describe the evolution of provenance and tectonic setting. Many factors influence sediment composition, namely, source rock composition, chemical weathering, climate, transport burial, and diagenesis. As the sediment composition changes through time, the geochemical characteristics of the sediment can be used to understand its geologic history. The geochemical characteristics of clastic sedimentary rocks are useful in determining the depositional setting and its associated provenance. Although many different studies have used geochemical discriminants to evaluate provenance and tectonic settings, none have used a defined geochemical method. This study evaluates the present-day geochemical approaches to see which, if any, are the most useful.
Стилі APA, Harvard, Vancouver, ISO та ін.
7

Asmussen, Pascal. "Insights from the Devonian Adavale Basin on the tectonic history of the Thomson Orogen." Thesis, Queensland University of Technology, 2020. https://eprints.qut.edu.au/200906/1/Pascal_Asmussen_Thesis.pdf.

Повний текст джерела
Анотація:
This research aims to advance our understanding of the expansion of the Australian continent during the Palaeozoic. Geological remnants of specific sedimentary basins in southwest Queensland and north-western NSW were used as focus sites. A novel multi-method approach used sediment compositional information and Uranium-Lead mineral dating in combination with novel statistical methods to constrain the relative timing, sediment pathways and connectivity of these basins. The research showed that although a major period of stabilisation of the Australian continent had occurred by the beginning of the Devonian, approximately 400 million years ago, the new sedimentary basins were not yet directly connected.
Стилі APA, Harvard, Vancouver, ISO та ін.
8

Becker, Thomas Patrick. "PALEOGEOGRAPHIC AND TECTONIC IMPLICATIONS OF THE LATE PALEOZOIC ALLEGHANIAN OROGEN DEVELOPED FROM ISOTOPIC SEDIMENTARY PROVENANCE PROXIES FROM THE APPALACHIAN FORELAND BASIN." UKnowledge, 2005. http://uknowledge.uky.edu/gradschool_diss/367.

Повний текст джерела
Анотація:
The Alleghanian orogeny was a collision between the Gondwanan and Laurentian continents that produced the Pangean supercontinent. Mechanical and kinematic models of collisional orogens are believed to follow a critical taper geometry, where the tectonic imbrication of continental crust begins nearest to the edge of continental plate and advances toward the craton in a break- forward sequence. Studies of shear zones within the Alleghanian collisional orogen, however, suggest that most of the early deformation was translational. Propagation of craton-directed thrusts into the foreland did not occur until the latest Pennsylvanian in the southern Appalachians, and the middle-late Permian in the central Appalachians. Radiometric sedimentary provenance proxies have been applied to the late Mississippian-early Permian strata within the Appalachian foreland basin to determine the crustal composition and structural evolution of the orogen during the continental collision. U-Pb ages of detrital zircons from the early to middle Pennsylvanian sandstones suggest that most of the detritus within the Appalachian basin was recycled from Mesoproterozoic basement and Paleozoic strata of the Laurentian margin. The presence of Archean and late Paleoproterozoic age detrital zircons is cited as evidence of recycling of the Laurentian syn-rift and passive-margin sandstones. Detrital zircon ages from early-middle Permian-age sandstones of the Dunkard Group do not contain any Archean or Paleoproterozoic detrital-zircon ages, implying a source of sediment with a much more restricted age population, possibly the igneous and metamorphic internides or middle Paleozoic sandstones from the Appalachian basin. The persistance of 360-400 Ma K/Ar ages of detrital white mica suggest that the sediment was supplied from a source that was exhumed during the Devonian Acadian orogeny. Detrital-zircon and detrital-white-mica ages from Pennsylvanian-age sandstones indicate that the late Paleozoic orogen did not incorporate any significant synorogenic juvenile crust. The 87Sr/86Sr ratios of middle Pennsylvanian-early Permian lacustrine limestones within the Appalachian basin show a slight enrichment through time, suggesting that labile 87Sr-rich minerals in the Alleghanian hinterland are being exposed. Stable isotopic data from the lacustrine limestones also corroborates that the Appalachian basin became much more arid through time.
Стилі APA, Harvard, Vancouver, ISO та ін.
9

Roe, Warren Paul. "Tertiary Sediments of the Big Hole Valley and Pioneer Mountains, Southwestern Montana: Age, Provenance, and Tectonic Implications." The University of Montana, 2010. http://etd.lib.umt.edu/theses/available/etd-08232010-181233/.

Повний текст джерела
Анотація:
Tertiary terrestrial sedimentary rocks of the Big Hole basin and Pioneer Mountains of southwestern Montana provide a record of regional extensional tectonism. Detailed observations of stratigraphy and sedimentology at widely scattered outcrops indicate the presence of paleosols, fine-grained debris flows, small alluvial channels, and rare fluvial deposits. U-Pb geochronology of detrital zircons and air-fall tuffs indicates the presence of Oligocene to Middle Miocene sedimentary rocks outcropping at the surface. Though the presence of detrital muscovite in several outcrops indicates derivation from the nearby 2-mica Chief Joseph pluton, a predicted ~75 Ma zircon population is not present: instead, a persistent peak of 70-72 Ma zircons is found throughout the basin, indicating the Chief Joseph pluton may have a younger emplacement age than is currently recognized. Simple physical models developed from Bouguer anomalies indicate the basin deepens and widens toward the south, which agrees with prior work suggesting Eocene initiation of extension in the Big Hole and places it in a class of extensional basins that formed in the early Tertiary. Late Cretaceous, Eocene, and Mesoproterozoic detrital zircon populations, along with consistently immature lithic sands, all indicate sediments were derived from local bedrock sources found around the rim of the modern Big Hole Valley. While these results indicate the Tertiary Big Hole basin resembled the modern basin, some later deformation may have cut off and reversed a paleodrainage flowing out of the southeastern portion of the basin, possibly leading to the modern configuration of the Big Hole River and the deep gorge it carves across the eastern Pioneer Mountains.
Стилі APA, Harvard, Vancouver, ISO та ін.
10

LaMaskin, Todd Allen. "Stratigraphy, provenance, and tectonic evolution of Mesozoic basins in the Blue Mountains Province, eastern Oregon and western Idaho /." Connect to title online (ProQuest), 2009. http://proquest.umi.com/pqdweb?did=1790314181&sid=2&Fmt=2&clientId=11238&RQT=309&VName=PQD.

Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
Більше джерел

Книги з теми "Tectonic provenance"

1

Gruninger, Hans R. V. Provenance of North America: The kinematic resolution of the Earth tectonic history. 2nd ed. Geoscience International, 1998.

Знайти повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
2

Martens, Uwe C. Southern and Central Mexico: Basement Framework, Tectonic Evolution, and Provenance of Mesozoic-Cenozoic Basins. Unknown Publisher, 2021.

Знайти повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
3

Martens, Uwe, and Roberto Stanley Molina Garza, eds. Southern and Central Mexico: Basement Framework, Tectonic Evolution, and Provenance of Mesozoic–Cenozoic Basins. Geological Society of America, 2020. http://dx.doi.org/10.1130/spe546.

Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
4

Bream, Susan Elaine. Depositional environment, provenance, and tectonic setting of the Upper Oligocene Sooke formation, Vancouver Island, B.C. 1987.

Знайти повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
5

Ingersoll, Raymond V., Timothy F. Lawton, and Stephan A. Graham. Tectonics, Sedimentary Basins, and Provenance: A Celebration of the Career of William R. Dickinson. Geological Society of America, 2018. http://dx.doi.org/10.1130/spe540.

Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.

Частини книг з теми "Tectonic provenance"

1

Barbeau, David L. "Exhumational History of the Margins of Drake Passage from Thermochronology and Sediment Provenance." In Tectonic, Climatic, and Cryospheric Evolution of the Antarctic Peninsula, 35–49. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/2010sp000992.

Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
2

Velmurugan, K., J. Madhavaraju, V. Balaram, A. Ramachandran, S. Ramasamy, E. Ramirez-Montoya, and J. C. Saucedo-Samaniego. "Provenance and Tectonic Setting of the Proterozoic Clastic Rocks of the Kerur Formation, Badami Group, Mohare Area, Karnataka, India." In Society of Earth Scientists Series, 239–69. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-89698-4_11.

Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
3

Prakash, Satya, Vivek P. Malviya, J. P. Verma, and Ravi K. Umrao. "Geochemistry and Petrological Studies of the Mesoproterozoic Glauconitic Sandstone, Semri Group, Vindhyan Basin, India: Implications for Paleoweathering, Provenance and Tectonic Setting." In Geochemical Treasures and Petrogenetic Processes, 353–73. Singapore: Springer Nature Singapore, 2022. http://dx.doi.org/10.1007/978-981-19-4782-7_13.

Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
4

Steidtmann, James R., and James G. Schmitt. "Provenance and Dispersal of Tectogenic Sediments in Thin-Skinned, Thrusted Terrains." In Frontiers in Sedimentary Geology, 353–66. New York, NY: Springer New York, 1988. http://dx.doi.org/10.1007/978-1-4612-3788-4_18.

Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
5

Nagarajan, R., J. S. Armstrong-Altrin, F. L. Kessler, and J. Jong. "Petrological and Geochemical Constraints on Provenance, Paleoweathering, and Tectonic Setting of Clastic Sediments From the Neogene Lambir and Sibuti Formations, Northwest Borneo." In Sediment Provenance, 123–53. Elsevier, 2017. http://dx.doi.org/10.1016/b978-0-12-803386-9.00007-1.

Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
6

Parker, Stuart D., and Marc S. Hendrix. "Detrital zircon record of the Mesoproterozoic Belt basin and implications for horizontal and vertical tectonic models." In In the Footsteps of Warren B. Hamilton: New Ideas in Earth Science. Geological Society of America, 2022. http://dx.doi.org/10.1130/2021.2553(14).

Повний текст джерела
Анотація:
ABSTRACT It is debated whether plate tectonics (horizontal tectonics) or single-lid tectonics (vertical tectonics) dominated the Mesoproterozoic Era. Either rifting of the Nuna/Columbia supercontinent or a localized vertical subsidence and tectonism mechanism within a single tectonic plate is likely recorded in Mesoproterozoic basins. This study summarizes detrital zircon samples from the Mesoproterozoic Belt and Purcell Supergroups and Lemhi subbasin of the western United States and Canada and tests competing rift and intracratonic basin models. Rift models take the observed detrital zircon trends to mean that a non-Laurentian (ca. 1.6–1.5 Ga) detrital zircon component becomes completely absent higher in the section, signifying rifting of the Nuna/Columbia supercontinent at ca. 1.4 Ga. Intracratonic models acknowledge this observed shift in provenance but interpret a long-lived intracratonic setting for the basin following an earlier failed rifting event. The fundamental question is whether the Belt basin represents a failed or successful rift. We used statistical comparison of 72 detrital zircon signatures, reported in the literature and presented in this study, to test the rift model. Samples are not evenly distributed across the basin or its stratigraphy. Non-Laurentian grains are spatially restricted to the northwest part of the basin but are present in all groups, suggesting that the apparent loss of the non-Laurentian population is an artifact of sampling bias. Like stratigraphic boundaries and facies changes, mixing trends are gradual, not sharp or sudden, signifying progressive reworking of Proterozoic zircons and transport from all sides. Archean zircons are localized near the edges of Archean blocks, signifying local down-dropping along cratonic margins. The rift model is therefore rejected in favor of the intracratonic model for the Belt basin on the basis of variable mixing between non-Laurentian and Laurentian sources in both pre–Missoula Group and Missoula Group strata. Far away from plate margins, sediment incrementally filled topographic depressions created by densified and thinned Proterozoic crustal blocks, resulting in vertical down-dropping along preexisting sutures with neighboring Archean blocks. More systematic detrital zircon studies are needed in order to accurately quantify provenance trends in space and time. Continued investigation of the Belt basin may reveal underappreciated or unrecognized vertical tectonic processes that may explain Mesoproterozoic rocks more accurately.
Стилі APA, Harvard, Vancouver, ISO та ін.
7

Clements, Benjamin, Inga Sevastjanova, Robert Hall, Elena A. Belousova, William L. Griffin, and Norman Pearson. "Detrital zircon U-Pb age and Hf-isotope perspective on sediment provenance and tectonic models in SE Asia." In Mineralogical and Geochemical Approaches to Provenance. Geological Society of America, 2012. http://dx.doi.org/10.1130/2012.2487(03).

Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
8

A. Akinyemi, Segun, Olajide F. Adebayo, Henry Y. Madukwe, Adeyinka O. Aturamu, and Olusola A. OlaOlorun. "Mineralogy and Geochemistry of Shales of Mamu Formation in Nigeria: Effects of Deposition, Source Rock, and Tectonic Background." In Geochemistry and Mineral Resources. IntechOpen, 2022. http://dx.doi.org/10.5772/intechopen.102454.

Повний текст джерела
Анотація:
Study of lithofacies identification, geochemical characterization of shales is vital to the provenance, paleoweathering, and tectonic setting reconstruction. The combination of morphological analysis, bulk chemical analysis and in-situ multi-element analysis was used to investigate the provenance, source area weathering, and depositional setting of outcropped Maastrichtian shale sequence of the Mamu Formation, Anambra Basin in Nigeria. Ten representative shale samples were examined by scanning electron microscopy/energy dispersive spectroscopy (SEM/EDS). Geochemical analysis was performed by X-ray fluorescence (XRF) Spectroscopy and Laser Ablation-Induced Coupled Plasma Mass Spectrometry (LA-ICPMS) techniques. The structural and morphological development of kaolinite in the outcropped shale samples of Mamu Formation is due to mechanical disintegration during transportation and re-deposition. Major oxides such as SiO2, Al2O3 and Fe2O3 constitute greater than 86% of the bulk composition. The weathering indices suggest highly weathered source materials. The plot of Cr versus Ni indicated the studied samples are Late Archean shale. Binary plots of trace elements suggest derivation from acidic or felsic sources rather than intermediate or basic source rocks. Ternary plot of Na2O + K2O, SiO2/10 and CaO + MgO indicated multiple sources such as felsic igneous rocks or recycled residues of quartz-rich. Tectonic discrimination diagram depict a typical Passive Margin field.
Стилі APA, Harvard, Vancouver, ISO та ін.
9

Welch, J. L., B. Z. Foreman, D. Malone, and J. Craddock. "Provenance of early Paleogene strata in the Bighorn Basin (Wyoming, USA): Implications for Laramide tectonism and basin-scale stratigraphic patterns." In Tectonic Evolution of the Sevier-Laramide Hinterland, Thrust Belt, and Foreland, and Postorogenic Slab Rollback (180–20 Ma). Geological Society of America, 2022. http://dx.doi.org/10.1130/2022.2555(09).

Повний текст джерела
Анотація:
ABSTRACT The Bighorn Basin (Wyoming, USA) contains some of the most extensively exposed and studied nonmarine early Paleogene strata in the world. Over a century of research has produced a highly resolved record of early Paleogene terrestrial climatic and biotic change as well as extensive documentation of spatiotemporal variability in basin-scale stratigraphy. The basin also offers the opportunity to integrate these data with the uplift and erosional history of the adjacent Laramide ranges. Herein, we provide a comprehensive provenance analysis of the early Paleogene Fort Union and Willwood Formations in the Bighorn Basin from paleocurrent measurements (n > 550 measurements), sandstone compositions (n = 76 thin sections), and U-Pb detrital zircon geochronology (n = 2631 new and compiled age determinations) obtained from fluvial sand bodies distributed widely across the basin. Broadly, we observed data consistent with (1) erosion of Mesozoic strata from the Bighorn and Owl Creek Mountains and transport into the eastern and southern basin; (2) erosion of Paleozoic sedimentary cover and crystalline basement from the Beartooth Mountains eastward into the northern Bighorn Basin; (3) conglomeratic fluxes of sediment from the Teton Range or Sevier fold-and-thrust belt to the southwestern Bighorn Basin; and (4) potential sediment provision to the basin via the Absaroka Basin that was ultimately derived from more distal sources in the Tobacco Root Mountains and Madison Range. Similar to previous studies, we found evidence for a system of transverse rivers contributing water and sediment to an axial river system that drained north into southern Montana during both the Paleocene and Eocene. Within our paleodrainage and provenance reconstruction, the basin-scale patterns in stratigraphy within the Fort Union and Willwood Formations appear to have been largely driven by catchment size and the lithologies eroded from the associated highlands. Mudrock-dominated strata in the eastern and southeastern Bighorn Basin were caused by comparably smaller catchment areas and the finer-grained siliciclastic strata eroded from nearby ranges. The conglomeratic and sand-dominated strata of the southwestern area of the Bighorn Basin were caused by large, braided fluvial systems with catchments that extended into the Sevier thrust belt, where more resistant source lithologies, including Neoproterozoic quartzites, were eroded. The northernmost early Paleogene strata represent the coalescence of these fluvial systems as well as rivers and catchments that extended into southwestern Montana that contained more resistant, crystalline lithologies. These factors generated the thick, laterally extensive fluvial sand bodies common in that area of the basin. When combined with provenance patterns in adjacent Laramide basins, our data indicate asymmetric unroofing histories on either side of the Bighorn and Owl Creek Mountains. The Powder River Basin to the east of the Bighorn Mountains displays a clear Precambrian crystalline provenance, and the Wind River Basin to the south of the Owl Creek Mountains displays provenance similarities to Lower Paleozoic strata, in contrast to provenance in the Bighorn Basin, which indicates less substantial unroofing. We infer that the differing unroofing histories are due to the dominant vergence direction of the underlying basement reverse faults. Overall, this provenance pattern persisted until ca. 50 Ma, when more proximal igneous and volcaniclastic units associated with the Absaroka and Challis volcanics became major sediment sources and the Idaho River system became the dominant transport system in the area.
Стилі APA, Harvard, Vancouver, ISO та ін.
10

ALGAR, SAM, EILEEN C. HEADY, and JAMES L. PINDELL. "FISSION-TRACK DATING IN TRINIDAD: IMPLICATIONS FOR PROVENANCE, DEPOSITIONAL TIMING AND TECTONIC UPLIFT." In Paleogeographic Evolution and Non-Glacial Eustacy, Northern South America, 111–28. SEPM (Society for Sedimentary Geology), 1998. http://dx.doi.org/10.2110/pec.98.58.0111.

Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.

Тези доповідей конференцій з теми "Tectonic provenance"

1

Fox, Nicholas R., David W. Mogk, David W. Bowen, David R. Lageson, and Paul A. Mueller. "THE MESOPROTEROZOIC LAHOOD FORMATION: PROVENANCE AND TECTONIC ENVIRONMENT OF DEPOSITION." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-283015.

Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
2

Jenchen, Uwe, María de Jesús Martínez López, Juan Moisés Casas Peña, Juan Alonso Ramírez Fernández, Fernando Velasco Tapia, Juan Carlos Montalvo Arrieta, and Carita Augustsson. "THE LAS DELICIAS FM., COAHUILA, MEXICO: PROVENANCE AND TECTONIC SETTING." In 54th Annual GSA South-Central Section Meeting 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020sc-343643.

Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
3

Okiotor, Michael Edirin, and EDeh Desiree Ogueh. "Geochemical Characteristics of the Campano-Maastrictian Sediments of the Anambra Basin, Southeastern Nigeria - Implication For Provenance, Paleodepositional Environment, Maturity and Tectonic Setting." In SPE Nigeria Annual International Conference and Exhibition. SPE, 2021. http://dx.doi.org/10.2118/207170-ms.

Повний текст джерела
Анотація:
Abstract The present study investigates the Anambra Basin shales to determine the provenance and maturity of the sediments using standard geochemical techniques. Twelve (12) representative samples recovered from shale sequences of The Mamu Formation and Nkporo Group of The Anambra Basin were studied to determine the sediment provenance, paleoenvironment, diagenetic conditions, maturity as well as the tectonic setting. To consider in detail and establish the inherent constituents of the Major minerals, Trace and Rare Earth elements, Inductively Coupled Plasma Mass Spectrometry (ICP-MS) analyses techniques was employed. The detrital minerals determined are Al2O3 (18.27% and 21.16%), TiO2 (1.73% and 1.63%) and Fe2O3 (2.78% \ and 2.85%), for Nkporo Group and Mamu Formation respectively. The enrichment of SiO2, Al2O3 and TiO2 (1.14, 1.94, 3.67 respectively) supported by Chemical Index of Alteration (CIA) of 93.54 & 39.55 and Rb/Sr ratio of 0.57 & 0.40, indicate that the Anambra Basin sediments are matured. TiO2/AL2O3 binary plots, Th/Co Vs La/Sc crossplots, Th-Sc-Zr triplots and Cr, Ni concentration suggest mixed provenance of felsic to mafic source rocks for these sediments. From the log (K2O/Na2O) Vs SiO2 crossplots, a passive margin tectonic setting was determined for these sediments.
Стилі APA, Harvard, Vancouver, ISO та ін.
4

Casas Peña, Juan Moisés, Eduardo Alejandro Alemán Gallardo, Juan Alonso Ramírez Fernández, Fernando Velasco Tapia, Carita Augustsson, Bodo Weber, Dirk Frei, and Uwe Jenchen. "THE PALEOZOIC SEDIMENTARY SEQUENCE OF TAMATÁN BASIN, NE MEXICO: PROVENANCE AND TECTONIC SETTING." In 54th Annual GSA South-Central Section Meeting 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020sc-343526.

Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
5

Jones, Adam, and Daniel M. Sturmer. "TECTONIC SUBSIDENCE ANALYSIS AND SEDIMENT PROVENANCE EVOLUTION OF THE LATE PALEOZOIC OQUIRRH BASIN, UTAH." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-321379.

Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
6

KORALAY, Demet Banu. "GEOCHEMISTRY FOR THE PLIOCENE CARBONACEOUS ROCKS FROM SOUTHEASTERN DENIZLI: PROVENANCE SIGNATURE AND TECTONIC SETTING." In 19th SGEM International Multidisciplinary Scientific GeoConference EXPO Proceedings. STEF92 Technology, 2019. http://dx.doi.org/10.5593/sgem2019/1.1/s01.026.

Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
7

Saylor, Joel E., Nicolas Bartschi, Thomas J. Lapen, Mike D. Blum, Bridget S. Pettit, and Ross A. Andrea. "TECTONIC CONTROLS ON LATE CRETACEOUS SEDIMENT PROVENANCE AND STRATIGRAPHIC ARCHITECTURE IN THE BOOK CLIFFS, UTAH." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-297252.

Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
8

Jaret, Steven, Nicholas D. Tailby, Keiji Hammond, Denton Ebel, Kathleen Wooton, and E. Troy Rasbury. "PROVENANCE, TECTONIC HISTORY, AND GEOCHEMISTRY OF THE MANHATTAN AND HARTLAND SCHISTS IN NEW YORK CITY." In GSA Connects 2021 in Portland, Oregon. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021am-370151.

Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
9

Taghdisi Nikbakht, S., Y. Nasiri, P. Rezaee, and R. Moussavi-Harami. "Provenance and Tectonic Setting of Early Permian Strata in the Kalmard Area, Central Iran Zone." In 83rd EAGE Annual Conference & Exhibition. European Association of Geoscientists & Engineers, 2022. http://dx.doi.org/10.3997/2214-4609.202210808.

Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
10

Ofili, Sylvester, Alvar Soesoo, Elena G. Panova, Rutt Hints, Sigrid Hade, and Leho Ainsaar. "RECONSTRUCTING THE PROVENANCE, TECTONIC SETTING AND PALEOWEATHERING OF LOWER PALEOZOIC BLACK SHALES FROM NORTHERN EUROPE." In GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-376758.

Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
Також вас можуть зацікавити розширені добірки на тему "Tectonic provenance" для конкретних типів джерел:
Статті в журналах Дисертації
Ми пропонуємо знижки на всі преміум-плани для авторів, чиї праці увійшли до тематичних добірок літератури. Зв'яжіться з нами, щоб отримати унікальний промокод!

До бібліографії