scholarly journals Syncontractional deposition of the Cretaceous Newark Canyon Formation, Diamond Mountains, Nevada: Implications for strain partitioning within the U.S. Cordillera

Geosphere ◽  
2020 ◽  
Vol 16 (2) ◽  
pp. 546-566 ◽  
Author(s):  
Russell V. Di Fiori ◽  
Sean P. Long ◽  
Anne C. Fetrow ◽  
Kathryn E. Snell ◽  
Joshua W. Bonde ◽  
...  
Keyword(s):  
Middle Part ◽  
Zircon Geochronology ◽  
Thrust Belt ◽  
Strain Partitioning ◽  
The West ◽  
Upper Paleozoic ◽  
Fault Propagation Fold ◽  
Mountain Belts ◽  
The U.S ◽  
Cretaceous Deposits

Abstract The timing of deformation and deposition within syntectonic basins provides critical information for understanding the evolution of strain in mountain belts. In the U.S. Cordillera, contractional deformation was partitioned between the Sevier thrust belt in Utah and several structural provinces in the hinterland in Nevada. One hinterland province, the Central Nevada thrust belt (CNTB), accommodated up to ∼15 km of shortening; however, in most places, this deformation can only be bracketed between Permian and Eocene. Cretaceous deposits of the Newark Canyon Formation (NCF), which are sparsely exposed along the length of the CNTB, offer the opportunity to constrain deformation timing. Here, we present mapping and U-Pb zircon geochronology from the NCF in the Diamond Mountains, which demonstrate deposition of the NCF during proximal CNTB deformation. Deposition of the basal NCF member was under way no earlier than ca. 114 Ma, a tuff in the middle part of the section was deposited at ca. 103 Ma, and the youngest member was deposited no earlier than ca. 99 Ma. Intraformational angular unconformities and abrupt along- and across-strike thickness changes indicate that NCF deposition was related to growth of an east-vergent fault-propagation fold. Clast compositions define unroofing of upper Paleozoic sedimentary rocks, which we interpret as the progressive erosion of an anticline ∼10 km to the west. CNTB deformation was contemporaneous with shortening in the Sevier thrust belt, which defines middle Cretaceous strain partitioning between frontal and interior components of the Cordillera. Strain partitioning may have been promoted by renewed underthrusting during a period of high-flux magmatism.

A4. UNRWA, IMPACT OF THE FIRST PHASE OF THE SECURITY BARRIER ON THE QALQILYA, TULKARM, AND JENIN DISTRICTS, GAZA CITY, JULY 2003 (EXCERPTS).

2003 ◽  
Vol 33 (1) ◽  
pp. 153-160
Keyword(s):  
Civil Engineering ◽  
West Bank ◽  
The West ◽  
Full Report ◽  
The World ◽  
Aid Coordination ◽  
President Bush ◽  
Engineering Projects ◽  
The U.S

The separation wall, one of the largest civil engineering projects in Israel's history, has been criticized even by the U.S. administration, with Condoleezza Rice stating at the end of June 2003 that it ““arouses our [U.S.] deep concern”” and President Bush on 25 July calling it ““a problem”” and noting that ““it is very difficult to develop confidence between the Palestinians and Israel with a wall snaking through the West Bank.”” A number of reports have already been issued concerning the wall, including reports by B'Tselem (available at www.btselem.org), the UN Office for the Coordination of Humanitarian Affairs (available at www.palestinianaid.info), and the World Bank's Local Aid Coordination Committee (LACC; also available at www.palestinianaid.info). UNRWA's report focuses on the segment of the wall already completed and is based on field visits to the areas affected by the barriers, with a special emphasis on localities with registered refugees. Notes have been omitted due to space constraints. The full report is available online at www.un.org/unrwa.

The Gedan floristic assemblage from the Late Cretaceous deposits of the Kholchan Formation of the Okhotsk-Chukotka volcanogenic belt

Palaeobotany ◽  
2014 ◽  
Vol 5 ◽  
pp. 73-93 ◽  
Author(s):  
L. B. Golovneva ◽  
S. V. Shczepetov
Keyword(s):  
River Basin ◽  
Late Cretaceous ◽  
Middle Part ◽  
Isotopic Data ◽  
Volcanogenic Belt ◽  
Stratigraphic Position ◽  
Cretaceous Deposits

The Gedan floristic assemblage occurs from upper layers of the Kholchan Formation of the Okchotsk-Chukotka volcanogenic belt (OCVB). The locality is situated at the Gedan River in the middle part of the Arman River basin. The Gedan assemblage is composed of 6 taxa: Cladophlebis sp., Sphenobaiera sp., Ginkgo ex gr. adiantoides (Ung.) Heer, Taxodium amguemensis (Efimova) Golovn., Metasequoia sp., Pagiophyllum sp. The similarity of the Gedan floristic assemblage with the Karamken and the Khirumki floristic assemblages from the Kholchan Formation of the Okhotsk sector of the OCVB allows us to join them in the Kholchan flora. This flora is distinct from more ancient Arman flora, which dated as the Turonian-Coniacian and from younger Ola flora, which dated as the Santonian-early Campanian. The age of the Kholchan flora is estimated as the Coniacian on the basis of stratigraphic position, presence of Podozamites, Metasequoia and Quereuxia and also isotopic data. This flora is equivalent with the Chaun flora of Central Chukotka, with the Aleeki flora from the Villigha and Toomahni Rivers interfluve and with the Ulya flora from the southern part of the Okhotsk-Chukotka volcanogenic belt.

The Impact of Culture on Reactions to Promise Breaches: Differences Between East and West in Behavioral Integrity Perceptions

2016 ◽  
Vol 43 (2) ◽  
pp. 273-315 ◽  
Author(s):  
Ray Friedman ◽  
Ying-Yi Hong ◽  
Tony Simons ◽  
Shu-Cheng (Steve) Chi ◽  
Se-Hyung (David) Oh ◽  
...  
Keyword(s):  
Cultural Context ◽  
Work Life ◽  
Communication Style ◽  
The West ◽  
Behavioral Integrity ◽  
Cultural Contexts ◽  
East And West ◽  
Different Cultures ◽  
The Impact ◽  
The U.S

Behavioral integrity (BI)—a perception that a person acts in ways that are consistent with their words—has been shown to have an impact on many areas of work life. However, there have been few studies of BI in Eastern cultural contexts. Differences in communication style and the nature of hierarchical relationships suggest that spoken commitments are interpreted differently in the East and the West. We performed three scenario-based experiments that look at response to word–deed inconsistency in different cultures. The experiments show that Indians, Koreans, and Taiwanese do not as readily revise BI downward following a broken promise as do Americans (Study 1), that the U.S.–Indian difference is especially pronounced when the speaker is a boss rather than a subordinate (Study 2), and that people exposed to both cultures adjust perceptions of BI based on the cultural context of where the speaking occurs (Study 3).

STRUCTURE, STRATIGRAPHY, AND PALEONTOLOGY OF AN UPPER TRIASSIC SECTION ON THE WEST COAST OF BRITISH COLUMBIA

1965 ◽  
Vol 2 (5) ◽  
pp. 442-484 ◽  
Author(s):  
Donald Carlisle ◽  
Takeo Susuki
Keyword(s):  
British Columbia ◽  
Structural Information ◽  
Pillow Lava ◽  
Middle Part ◽  
Upper Triassic ◽  
Coast Range ◽  
Thermal Alteration ◽  
The West ◽  
Coastal British Columbia ◽  
Sedimentary Unit

The highly deformed section at Open Bay is one of the few good exposures of a thick sedimentary unit within the prebatholithic rocks along coastal British Columbia. It provides new structural information relating to emplacement of a part of the Coast Range batholith and it contains an important Upper Triassic fauna unusually well represented. Structural and paleontological analyses are mutually supporting and are purposely combined in one paper.Thirteen ammonite genera from 14 localities clearly substantiate McLearn's tentative assignment to the Tropites subbullatus zone (Upper Karnian) and suggest a restriction to the T. dilleri subzone as defined in northern California.Contrary to an earlier view, the beds are lithologically similar across the whole bay except for variations in the intensity of deformation and thermal alteration. Their contact with slightly older relatively undeformed flows is apparently a zone of dislocation. Stratigraphic thicknesses cannot be measured with confidence, and subdivision into "Marble Bay Formation" and "Open Bay Group" cannot be accepted. Open Bay Formation is redefined to include all the folded marble and interbedded pillow lava at Open Bay. Lithologic and biostratigraphic correlation is suggested with the lower middle part of the Quatsino Formation on Iron River, 24 miles to the southwest. Basalt flows and pillowed volcanics west of Open Bay are correlated with the Texada Formation within the Karmutsen Group.The predominant folding is shown to precede, accompany, and follow intrusion of numerous andesitic pods and to precede emplacement of quartz diorite of the batholith. Structural asymmetry is shown to have originated through gentle cross-folding and emplacement of minor intrusives during deformation.

Survey Research on Legal System of Floating Residence and on Management of Water Utilization in the United States: Case Study on Seattle, Washington and Sausalito, California

2018 ◽  
Author(s):  
Daisuke Dobashi ◽  
Akio Kuroyanagi ◽  
Ryo Sugahara
Keyword(s):  
United States ◽  
Survey Research ◽  
The United States ◽  
Web Survey ◽  
The West ◽  
Effective Utilization ◽  
Water Utilization ◽  
Building Standards ◽  
The U.S

Effective utilization of oceanic space in Japan is just recent compared to U.S. Since the end of 19th century, water utilization and management for residence constructed on lake was promoted in U.S. It is then the aim of this paper to comprehend the laws and regulations for floating residence as well as water utilization and management of United States. Through web survey, each State in United States will be searched if there are existing laws and regulation on floating residence. After searching and reading all conditions of the U.S. States regarding laws and regulation as well as legal positions on floating residence, two states in the west coast of U.S: Seattle in Washington and Sausalito, California are chosen for this study. Floating residence in U.S. are divided into two; the Floating Homes and Houseboats. Floating Homes are handled by law the same with homes built in land while Houseboats are treated as type of ship. The State managing the water will lease it to the private sector, then, building of Floating Home will be carried out. Furthermore, design and construction of Floating Homes follow the building standards of the counties and cities where it will be built.

scholarly journals THE ROLE OF THE MIDDLE EAST INVESTMEN INITIATIVE (MEII) IN DEVELOPMENT IN THE WEST BANK, PALESTINE IN THE U.S.-PALESTINE PARTNERSHIP (UPP) FRAMEWORK

2018 ◽  
Author(s):  
Presya Ramadhan
Keyword(s):  
Middle East ◽  
Private Sector ◽  
West Bank ◽  
Public Private Partnership ◽  
The West ◽  
Private Partnership ◽  
Security Issues ◽  
Private Sector Investment ◽  
The U.S

This paper examines the role of Middle East Investment Initiative (MEII) in development in the West Bank, Palestine in the U.S.-Palestine Partnership (UPP) framework. Answering the question of how the role of the Middle East Investment Initiative (MEII) in development in Palestine in the US-Palestine Partnership (UPP) framework and how the contribution of Public-Private Partnership (PPP) to development in Palestine, the author's thesis statement is that amid diplomatic and territorial disputes, The Middle East Investment Initiative (MEII) as a public-private partnership becomes the main channel for collecting and channeling development assistance such as resources and private sector investment that can benefit the West Bank and bring prosperity to people Palestinians. While the private sector such as the Middle East Investment Initiative (MEII) cannot do much to address diplomacy or security issues, the private sector can play an equally important role through the contribution of resources and investment to conflict areas such as Palestine to help economic development In the West Bank, Palestine.

scholarly journals Types of river sources of the thin-grained aluminosilicaclastics for the Jurassic and lower cretaceous deposits of the West Siberian megabasin

2021 ◽  
Vol 63 (4) ◽  
pp. 52-61
Author(s):  
A. V. Maslov
Keyword(s):  
Lower Cretaceous ◽  
The Urals ◽  
River Systems ◽  
The West ◽  
Rock Composition ◽  
Fine Grained ◽  
The North ◽  
Catchment Areas ◽  
Cretaceous Deposits ◽  
West Siberian Basin

Background. The lithogeochemical features of fine-grained detrital rocks (mudstones, shales, and fine-grained siltstones) allow, with a certain degree of success, the main parameters of the formation of sedimentary sequences to be reconstructed. These parameters include (primarily in terms of their REE and Th systematics) the types of river systems supplying thin terrigenous suspension in the sedimentation area: the rivers of the 1st category – large rivers with a catchment area of more than 100,000 km2; 2nd category – rivers feeding on the products of erosion of sedimentary deposits; 3rd category – rivers draining mainly igneous and metamorphic rocks; and 4th category – rivers carrying erosion products of volcanic associations.Aim. To reveal, based on the analysis of interrelationships between such parameters as (La/Yb)N, Eu/Eu* and the Th content, the types of river systems that fed the Jurassic and Lower Cretaceous deposits of the Shaim oil and gas region (OGR) (Sherkalinsky, Tyumen, Abalak and Mulymya formations) and the region of the North Pokachevsky field of the Shirotnoe Priobye region (Sherkalinsky, Tyumen and Bazhenov formations, Lower Cretaceous deposits).Materials and methods. The ICP MS data for almost 100 samples of mudstones and fine-grained clayey siltstones were used to analyse the features of distribution of lanthanides and Th in the Jurassic and Lower Cretaceous clayey rocks of the Shaim OGR and the area of the North Pokachevsky deposits. Individual and average composition points for formations, members and layers were plotted on the (La/Yb)N-Eu/Eu*, (La/Yb)N–Th diagrams developed by us with classification areas of the composition of fine suspended material of modern rivers of different categories.Results and conclusion. The results presented in the article showed that during the formation of the deposits of the Shaim OGR in the Early and Middle Jurassic, erosion affected either mainly sedimentary formations or paleo-catchment areas that were very variegated in their rock composition. In the Late Jurassic, the source area was, most likely, a volcanic province, composed mainly of igneous rocks of the basic composition, and located within the Urals. This conclusion suggested that the transfer of clastic material from the Urals to the Urals part of the West Siberian basin “revived” much earlier than the Hauterivian. The Jurassic-Lower Cretaceous section of the vicinity of the North Pokachevsky field was almost entirely composed of thin aluminosilicaclastics formed due to the erosion of volcanic formations. These volcanic formations were located, as followed from the materials of earlier performed paleogeographic reconstructions, probably within the Altai-Sayan region or Northern Kazakhstan. Thus, the supply of detrital material in the considered territories of the West Siberian basin had a number of significant differences in the Jurassic and early Cretaceous.

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