Sediment Provenance: Influences on Compositional Change from Source to Sink provides a thorough and inclusive overview that features data-based case studies on a broad range of dynamic aspects in sedimentary rock structure and deposition. The following concepts are outlined K E Y W O R D S cosmogenic nuclides dating (26 Al/ 10 Be), incipient rifting, intracratonic morphodynamics, Okavango Basin, provenance analyses (Pb, Sr, Nd isotopes). Geochemically, the sediments were classified as litharenites and the Index of Compositional Variability (ICV) varied between 1.4 and 2.0, indicating low compositional and mineralogical maturity. Moreover, when dealing with detrital heavy minerals including single-grain chemical analysis one has to take into account the grain-size control on sediment composition including single-grain compositional variations. The factors controlling the composition of clastic sediments, and associated biases, have been extensively studied in the past and included in landmark special volumes (Johnsson and Basu, 1993;Valloni and Basu, 2003;von Eynatten et al., 2012a;Caracciolo et al., 2016a;Weltje et al., 2018) and reviews from Suttner (1974), Basu (1985aBasu ( , 1985b, Pettijohn et al. Oligocene sediment pathways from source to sink crossed further crystalline basement units and sedimentary covers before entering the basin from the southeast. confirms the application and the importance of heavy minerals in sedimentary provenance analysis. The work illustrates how the current, state-of-the-art technology can be effectively utilized to address ongoing challenges in petroleum geoscience. Both the advantages and limitations of each analytical tool are explored, and best practices for successful analytical workflows are discussed in light of a full integration into SRS research. The prolonged convergence along the Southeast Asian margin from the Mesozoic to Cenozoic shaped the region into a complex tectonic collage of microblocks of diverse origin and evolutionary history. The macroscopic provenance analysis (gravel composition analysis) is a very useful tool for the characterization of changes in sedimentary sources through time, Since the 1980ies detrital garnet chemistry is extensively used as a tool in sedimentary provenance studies, yet there is no clear-cut understanding of what garnet type originates from which host l, The Palaeozoic rocks of the Dingle Peninsula provide a record of the evolution of the Caledonides, Acadides and Variscides. The timing and nature of the provenance change recorded in the Drummond Basin are consistent with it being driven by the contemporaneous but far-field intraplate Alice Springs Orogeny of central Australia. Sm and Nd reservoirs within the shale change considerably with progressive diagenesis. To investigate potential metamorphic sources, 18 detrital rutile samples were analysed for a total of 1,431 analyses. The succession ranges from Early Ordovician deep-water sediments, through Silurian shallow marine to non-marine sediments and volcanic rocks to an Old Red Sandstone (ORS) succession topped by Carboniferous marine shales. The older rocks record Caledonian processes on the margin of Avalonia during Early Ordovician time and convergence then soft collision with Laurentia during Silurian time. and INGERSOLL, R.V. After Iapetus closure, changes in the tectonic regime are believed to be a result of adjustments in the geometry of subduction of the Rheic Ocean. The aim of this project is (1) to study the grain-size dependence of garnet composition and (2) establish new interpretation schemes that allow for better discrimination of the detrital garnet minerals and their potential host rock lithologies based on robust probabilistic models. Provenance studies utilizing these new dating methods can provide valuable insights into the depositional environments of these rocks which in turn help describe the tectonic evolution of the Lake Superior region. Journal Sedimentary Petrology 55:340–346. Sm-Nd analyses of sandstones and shales from the Wilcox Group (Upper Paleocene-Lower Eocene) suggest that the whole rock Sm-Nd signature is changed by burial diagenesis. Vertical provenance changes generally reflect either basin-forming tectonic processes, climate variations or far-field orogenies that can generate large-volumes of compositionally distinct sediment that overwhelms local sediment supply. Chemically, they are related to the sand fraction of continental platform cover. This study uses zircon and apatite U‐Pb geochronology, apatite trace elements, zircon‐tourmaline‐rutile indices and petrographic observations to investigate the sedimentary history of mineralogically mature mid‐Carboniferous sandstones of the Tullig Cyclothem, Clare Basin, western Ireland. Resemblance of the sediment compositions to mean compositions from Higher Himalaya crystalline rocks pointed to these being potential source rocks but with components from a mafic source also present. The samples are from the San Marcos arch, south-central Texas, at depths ranging from outcrop to 15,000 feet. However, the multi‐proxy approach also helps constrain the sedimentary history, and suggests that not all grain populations were derived directly from their original source. The rutile data are dominated by Pacific-Gondwanan ages, with a minor ~1,547 Ma detrital population appearing mid-succession. This study highlights the need for a multi‐proxy provenance approach to constrain sedimentary recycling, particularly in compositionally mature sandstones, as the use of zircon geochronology alone would have led to erroneous provenance interpretations. These areas represent an uplifted and variably dissected Mesozoic magmatic arc. Results of mineralogy and geochemistry of the Neogene siliciclastic deposits of the Tukau and Belait formations were studied with the objectives to identify the provenance, estimate the intensity of continental weathering and infer the influence of Previous studies interpreted a transport system dominated by relatively low-energy meandering rivers where the packages of conglomerate were interpreted as channel lags flanked by sandstone and siltstone being point bar and overbank deposits. A classification scheme for volcanic grains, involving five classes dependent on palaeovolcanic and neovolcanic sources. 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