The great majority of the activities are thus using that port for imports or exports.

Rare earth and major elements, detrital zircon ages, sandstone petrography and garnet composition, suggest a dominantly Ordovician – Silurian aged felsic and metasedimentary hinterland.

Significant subsidence only occurs if the deep crust is relatively strong and the density anomaly is located within the crust.

hinterland : The tributary (or catchment) area of a port, from which materials for export are collected and through which imports are distributed: its complementary area — connected to the port by ship — is termed the foreland.

The core of a mountain belt, often characterized by rocks of high metamorphic grade and ductile deformation histories is the hinterland of the range. To produce surface deflection over a width of ~100 km, the near-surface rocks must be relatively weak.Department of Physics, University of Alberta, Edmonton, AB T6G 2E1, Canada.Search for other works by this author on:Department of Geosciences, University of Arizona, Tucson, Arizona 85721, USA.You do not currently have access to this chapter.You could not be signed in. A continuous, 800 m thick, organic rich and highly oil-prone, lacustrine section was investigated in outcrop and in a continuously cored section. By continuing you agree to the.Copyright © 2020 Elsevier B.V. or its licensors or contributors.ScienceDirect ® is a registered trademark of Elsevier B.V.Hinterland setting and composition of an Oligocene deep rift-lake sequence, Gulf of Tonkin, Vietnam: Implications for petroleum source rock deposition.© 2019 Elsevier Ltd. All rights reserved.https://doi.org/10.1016/j.marpetgeo.2019.08.022. Hinterland. George G. Chisholm ( Handbook of Commercial Geography, 1888) transcribed the German word hinterland (land in back of), as hinderland, and used it to refer to the backcountry of a port or coastal settlement.

• An area behind a coast or the shoreline of a river. Foreland and hinterland. Vision and context. Three types of deflection are observed: (1) >500 m subsidence, followed by uplift, (2) little subsidence, and (3) uplift followed by collapse.

Calcarenita: Roca sedimentaria formada por granos calizos de tamaño de arena. Great Britain was a model of imperial science and possessed a working consensus on doing geology that provided a framework for Logan and the Geological Survey. "Hinterland basin formation and gravitational instabilities in the central Andes: Constraints from gravity data and geodynamic models", Geodynamics of a Cordilleran Orogenic System: The Central Andes of Argentina and Northern Chile, Peter G. DeCelles, Mihai N. Ducea, Barbara Carrapa, Paul A. Kapp.The evolution of surface topography in an orogen provides information about the dynamics of the deep lithosphere.

Huilin Wang, Claire A. Currie, Peter G. DeCelles, 2015. Please check your email address / username and password and try again.BRIGID E. CHRISTISON, DARREN H. TANKE, JORDAN C. MALLON,This site uses cookies.

Please check your email address / username and password and try again.Department of Geosciences, University of Arizona, Tucson, Arizona, USA,Department of Geosciences, University of Arizona, Tucson, Arizona, USA, and Universitatea Bucuresti, Facultatea de Geologie Geofizica, Strada N. Balcescu Nr 1, Bucuresti, Romania.Attribution:You must attribute the work in the manner specified by the author or licensor (but not in any way that suggests that they endorse you or your use of the work).

Tropical leaching resulted in an extraordinary high phosphorus input into the lake that catalyzed a high organic productivity and promoted the generation of highly prolific, oil-prone source rocks. This promoted the establishment of a long-lived, deep lake favorable for source rock generation. Antwerp is one of the most important rail ports in Europe. In addition, heavy mineral and geochemical data document an unusually high content of detrital phosphate minerals in the investigated section indicative of a phosphate-rich hinterland. Orientations of ripple cross lamination in gravity flow sands indicate axial sediment transport along the graben. The Oligocene deep-lake succession formed in the Bach Long Vi Graben that connects the Beibuwan Basin with the Yinggehai-Song Hong Basin. The competition margins are areas where two or more ports are in competition.

Comparable petroleum source rocks are likely to exist in other ancient rift basins surrounded by small, phosphate-rich hinterlands sheltered from significant sediment input.We use cookies to help provide and enhance our service and tailor content and ads. Foreland and Hinterland-Based Regionalization. Two-dimensional numerical models are used to investigate the topographic expression associated with removal of a high-density lithosphere root. Rail . William Eagan; The Canadian Geological Survey: Hinterland Between Two Metropolises.Recognizing the 150th Anniversary of the foundation of the Geological Survey of Canada as an apt moment to assess and explore the historical context of the Survey, this paper examines the founding of the Survey, the role of William Logan as the first Director and the manner in which he shaped the structure and vocabulary of Canadian geology.

No Derivative works ‒ You may not alter, transform, or build upon this work. Petrography, detrital zircon U-Th-Pb geochronology and heavy mineral assemblages of sandstone intervals document a locally derived sediment source isolated from the Red River.

PubMed. William Eagan 1. Search for other works by this author on: This Site. The “Sunshine Coast” conjures up images of golden beaches, rocky islands and green mountains of the hinterland, and we could assume that this peaceful landscape results from a stable geological framework..

Emulating both metropolises, Logan borrowed from each in a dynamic interaction as he worked to develop a distinctive response to Canadian social and scientific needs.

This differential exhumation provides the first and minimum constraint on the long‐term throw rate (~0.6 km/m.y) of the Wenchuan‐Maoxian fault since the late Miocene.

C Cabalgamiento: Conjunto de capas rocosas de edad más antigua que se superponen sobre otras de edad más moderna por efecto de presiones laterales.

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