Dating thermal anomalies in sedimentary basins: the diagenetic history of clay minerals in the Triassic sandstones of the Paris Basin, France

Clay Minerals ◽  
1992 ◽  
Vol 27 (2) ◽  
pp. 211-226 ◽  
Author(s):  
J. R. Mossmann ◽  
N. Clauer ◽  
N. Liewig
Keyword(s):  
Clay Minerals ◽  
North Atlantic Ocean ◽  
Sedimentary Basins ◽  
Morphological Data ◽  
Burial Depth ◽  
Paris Basin ◽  
Hydrothermal Conditions ◽  
Thermal Anomalies ◽  
The North ◽  
History Of

AbstractRhaetian (Upper Triassic) sandy horizons were sampled from the Paris Basin from SW to NE, crosscutting the Rhaetian at different depths from outcrop in the NE to 2700 m in the centre of the basin. The smallest day sub-fractions (<0·2 μm) from the deepest samples consist mainly of illite and chlorite having a K-Ar age of 〜190 Ma. Both minerals probably formed under specific hydrothermal conditions at high temperature, but at a burial depth of only 500 m. This thermal event could represent an echo of the "crustal" breakdown of the Northwestern European craton during the opening of the North Atlantic Ocean. Two other generations of illite-smectite mixed-layers formed in the same Rhaetian horizons at somewhat lower temperatures about 150 and 80 Ma ago. The three generations of clay minerals could be characterized and dated because of combined mineralogical, crystallographical and morphological data supporting the dating attempts.

Black Magic in Modern Times

2019 ◽  
pp. 1-8
Author(s):  
Thomas Waters
Keyword(s):  
North Atlantic Ocean ◽  
Human Movement ◽  
Modern Times ◽  
The North ◽  
Large Island ◽  
History Of ◽  
The North Atlantic ◽  
Black Magic ◽  
Eastern Edge ◽  
Magical Beliefs

This chapter shows that the history of black magic in modern times is a cosmopolitan drama. Human movement rapidly accelerated from the nineteenth century. People, goods, technologies, and ideas began crossing the earth at a dizzying rate. Travellers took their magical beliefs abroad and encountered new mysticisms when they got there. Empires regulated their colonial subjects in all sorts of ways, including how they dealt with witches. Witchcraft became more international, though at the same time it remained fundamentally rooted in local circumstances. This means that, to understand modern witchcraft, one must combine a global orientation with a local focus. And an excellent place for that local focus is a large island, lying on the eastern edge of the North Atlantic Ocean: Britain.

The classic Wilson cycle revisited

2018 ◽  
Vol 470 (1) ◽  
pp. 19-38 ◽  
Author(s):  
Ian W. D. Dalziel ◽  
John F. Dewey
Keyword(s):  
North Atlantic ◽  
North Atlantic Ocean ◽  
Ocean Basin ◽  
Early Paleozoic ◽  
The North ◽  
History Of ◽  
Wilson Cycle ◽  
Mountain Chain ◽  
The 1960S ◽  
Opening And Closing

AbstractIn the first application of the developing plate tectonic theory to the pre-Pangaea world 50 years ago, attempting to explain the origin of the Paleozoic Appalachian–Caledonian orogen, J. Tuzo Wilson asked the question: ‘Did the Atlantic close and then reopen?’. This question formed the basis of the concept of the Wilson cycle: ocean basins opening and closing to form a collisional mountain chain. The accordion-like motion of the continents bordering the Atlantic envisioned by Wilson in the 1960s, with proto-Appalachian Laurentia separating from Europe and Africa during the early Paleozoic in almost exactly the same position that it subsequently returned during the late Paleozoic amalgamation of Pangaea, now seems an unlikely scenario. We integrate the Paleozoic history of the continents bordering the present day basin of the North Atlantic Ocean with that of the southern continents to develop a radically revised picture of the classic Wilson cycle The concept of ocean basins opening and closing is retained, but the process we envisage also involves thousands of kilometres of mainly dextral motion parallel with the margins of the opposing Laurentia and Gondwanaland continents, as well as complex and prolonged tectonic interaction across an often narrow ocean basin, rather than the single collision suggested by Wilson.

Late Neogene marine Ostracoda from Tjörnes, Iceland

1991 ◽  
Vol 65 (5) ◽  
pp. 767-794 ◽  
Author(s):  
Thomas M. Cronin
Keyword(s):  
North Atlantic ◽  
North Atlantic Ocean ◽  
Warm Water ◽  
Early Pleistocene ◽  
The North ◽  
East Greenland Current ◽  
Late Neogene ◽  
History Of ◽  
Western Side ◽  
Glacial Tills

On the western side of the Tjörnes Peninsula in northern Iceland exposures of fossiliferous marine sediments, basalts, and glacial tills record the climatic history of this region of the North Atlantic Ocean. Seventy-five marine ostracode species were recovered from the Pliocene Tjörnes sediments and Quaternary sediments known as the Breidavik beds. The ostracode assemblages contain many warm-water genera that do not inhabit Iceland today and indicate early to middle Pliocene (4.5–3.0 Ma) winter and summer bottom-water temperatures that averaged 5–6°C and 14–16°C, respectively (maximum 20°C in summer, rarely below 3°C in winter except during a brief cooling 3.5–3.2 Ma). An intensified North Atlantic Drift and a diminished or absent East Greenland Current account for warm-water oceanographic conditions at 66°N. Late Pliocene marine climates were cooler with winter and summer averages of about 9°C and 8°C. Early Pleistocene ostracode assemblages dated at 1.7–1.3 Ma contain extant arctic–subarctic species that indicate winter and summer temperatures of about − 1.5°C and 4–5°C. New speciesBensonocythere eirikssoni, Robertsonites williamsi, Hemicythere rekaensis, Thaerocythere mayburyae, Thaerocythere whatleyi, Leptocythere tjornesensis, Tetracytherura bardarsoni, andCytheromorpha einarssoniare described.

Clay minerals as records of temperature conditions and duration of thermal anomalies in the Paris Basin, France: a reply to the discussion by Spötl et al.

Clay Minerals ◽  
1996 ◽  
Vol 31 (2) ◽  
pp. 209-215 ◽  
Author(s):  
N. Clauer ◽  
J. R. O'Neil ◽  
S. Furlan ◽  
J. R. Mossmann
Keyword(s):  
Clay Minerals ◽  
Alternative Explanation ◽  
Thermal Evolution ◽  
Basic Data ◽  
Formation Temperature ◽  
Paris Basin ◽  
Thermal Anomalies ◽  
Temperature Conditions ◽  
The One ◽  
Clay Materials

AbstractSpötl et al. (1996) have re-examined studies published by us on clay materials of sandstones in the Paris Basin. They refute the XRD characterization, K-Ar dating and formation temperature of one of the interstratified illite-smectite phases identified and have provided an alternative explanation of the published results. However, the authors ignored some basic data provided in the publications under discussion, and they have not been able to explain readily why some of the data were discarded. Furthermore, part of their disagreement is unsubstantiated. We maintain that, on the basis of coherency and consistency of all the data obtained, as well as on independent published results, the most satisfactory interpretation for the thermal evolution of the Paris Basin is the one that we suggested in our publications.

scholarly journals Mineralogical Evolution of the Cretaceous Strata in the Songliao Basin, Northeastern China: Implications for Thermal History and Paleoenvironmental Evolution

Minerals ◽  
2021 ◽  
Vol 11 (10) ◽  
pp. 1101
Author(s):  
Tian Dong ◽  
Yuan Gao ◽  
He Huang ◽  
Xing Tian ◽  
Qian Yang ◽  
...  
Keyword(s):  
Clay Minerals ◽  
Thermal History ◽  
Environmental Changes ◽  
Thermal Evolution ◽  
Sedimentary Basins ◽  
Northeastern China ◽  
Songliao Basin ◽  
Published Data ◽  
Burial Depth ◽  
Geothermal Resources

The Songliao Basin in northeastern China is one of the largest and longest-lived Cretaceous sedimentary basins enriched in petroleum and geothermal resources worldwide. Although the modern Songliao Basin has a high geothermal gradient, the geological thermal history of the basin has not been well constrained. The SK-2 drilling program, as the second stage of the International Continental Drilling Project of Cretaceous Songliao Basin, is for recovering extensive Early Cretaceous terrestrial strata and providing valuable materials for decoding the mineralogical evolution and the paleoenvironmental changes. Here, we present whole-rock and clay mineralogical analysis on 72 core samples covering 3346–5705 m of the Shahezi Formation in the SK-2 borehole. The whole-rock minerals mainly include clay minerals, quartz, plagioclase, as well as some calcite, K-feldspar, siderite, and pyrite. The clay mineral assemblages include illite, chlorite, and illite–smectite interlayer minerals. Above 4500 m, clay minerals are dominated by illite and illite–smectite interlayers. Below 4500 m, more plagioclase, K-feldspar, and calcite are present, while illite–smectite interlayers are completely replaced by illite. The whole-rock and clay mineralogical evolution of the Shahezi Formation is primarily controlled by thermal diagenesis, although paleoenvironmental change may act as a minor contribution. Combined with published data from the Upper Cretaceous in SK-1 cores, we infer that Cretaceous greenhouse climatic and environmental changes left fingerprints on whole-rock and clay mineralogical assemblages and that the Songliao Basin reached a maximum burial depth and a peak of thermal evolution at the end of the Cretaceous.

scholarly journals A review of the Pan-African evolution of the Arabian Shield

GeoArabia ◽  
2002 ◽  
Vol 7 (1) ◽  
pp. 103-124 ◽  
Author(s):  
Pierre Nehlig ◽  
Antonin Genna ◽  
Fawzia Asfirane ◽  
C. Guerrot ◽  
J.M. Eberlé ◽  
...  
Keyword(s):  
Structural Evolution ◽  
Sedimentary Basins ◽  
Fault Zones ◽  
Fault System ◽  
Arabian Shield ◽  
Geologic History ◽  
Lower Paleozoic ◽  
The North ◽  
Pan African ◽  
History Of

ABSTRACT Recent fieldwork and the synthesis and reappraisal of aeromagnetic, geologic, structural, geochemical, and geochronologic data have provided a new perspective on the structural evolution and geologic history of the Arabian Shield. Although Paleoproterozoic rocks are present in the eastern part of the Shield, its geologic evolution was mainly concentrated in the period from 900 to 550 Ma during which the formation, amalgamation, and final Pan-African cratonization of several tectonostratigraphic terranes took place. The terranes are separated by major NW-trending faults and by N-, NW- and NE-oriented suture zones lined by serpentinized ultramafic rocks (ophiolites). Terrane analysis using the lithostratigraphy and geochronology of suture zones, fault zones, overlapping basins, and stitching plutons, has helped to constrain the geologic history of the Arabian Shield. Ophiolites and volcanic-arcs have been dated at between 900 and 680 Ma, with the southern terrane of Asir being older than the Midyan terrane in the north and the Ar Rayn terrane in the east. Final cratonization of the terranes between 680 and 610 Ma induced a network of anastomosing, strike-slip faults consisting of the N-trending Nabitah belt, the major NW-striking left-lateral transpressive faults (early Najd faults), lined by gneiss domes and associated with sedimentary basins, and N- to NE-trending right-lateral transpressive faults. Following the Pan-African cratonization, widespread alkaline granitization was contemporaneous with the deposition of the Jibalah volcanic and sedimentary rocks in transtensional pull-apart basins. Crustal thinning was governed by the Najd fault system of left-lateral transform faults that controlled the formation of the Jibalah basins and was synchronous with the emplacement of major E- to NW-trending dike swarms throughout the Arabian Shield. The extensional episode ended with a marine transgression in which carbonates were deposited in the Jibalah basins. Continuation of the thinning process may explain the subsequent deposition of the marine formations of the lower Paleozoic cover. Our interpretation of the distribution and chronology of orogenic zones does not correspond entirely to those proposed in earlier studies. In particular, the N-trending Nabitah and NW-trending Najd fault zones are shown to be part of the same history of oblique transpressional accretion rather than being two distinct events related to accretion and dispersion of the terranes.

scholarly journals The tribe Scrophularieae (Scrophulariaceae): A Review of Phylogenetic Studies

Hacquetia ◽  
2019 ◽  
Vol 18 (2) ◽  
pp. 337-347 ◽  
Author(s):  
Mehrshid Riahi ◽  
Farrokh Ghahremaninejad
Keyword(s):  
Phylogenetic Relationships ◽  
Molecular Data ◽  
Morphological Data ◽  
Hybrid Speciation ◽  
The North ◽  
Phylogenetic Studies ◽  
Phylogenetic Reconstructions ◽  
Data Collection And Analysis ◽  
History Of ◽  
Review Reports

Abstract Molecular data have been increasingly used to study the phylogenetic relationships among many taxa, including scrophs. Sometimes they have provided phylogenetic reconstructions that are in conflict with morphological data leading to a re-evaluation of long-standing evolutionary hypotheses. In this paper, we review reports of the recent knowledge of the phylogenetic relationships within Scrophularieae (2011–2017). The results of these analyses led to the following conclusions. (1) Species of Scrophularia have undergone one or more Miocene migration events occurred from eastern Asia to the North America with subsequent long dispersal and diversification in three main directions. (2) Allopolyploid and aneuploid hybrid speciation between Scrophularia species can occur, so hybridization and polyploidy have an important role for history of diversification. (3) The ancestral staminode type for the genus Scrophularia seems to be a large staminode. (4) Monophyly of the genus Verbascum with respect to the genus Scrophularia is strongly supported. (5) Oreosolen, is not monophyletic, because all accessions of Oreosolen were nested within Scrophularia. We discuss methods of data collection and analysis, and we describe the areas of conflict and agreement between molecular phylogenies.

Isomerization and aromatization of hydrocarbons in sedimentary basins formed by extension

1983 ◽  
Vol 120 (5) ◽  
pp. 417-470 ◽  
Author(s):  
A. S. Mackenzie ◽  
D. McKenzie
Keyword(s):  
Pannonian Basin ◽  
Sedimentary Basins ◽  
West Germany ◽  
Lower Saxony ◽  
Single Measure ◽  
The North ◽  
Aromatization Reaction ◽  
Different Temperatures ◽  
History Of ◽  
Reaction Constants

Summary. The reactions involved in oil generation are of great economic importance, but remain to be studied in detail. We have investigated the rates of three reactions which occur before and during the early stages of oil formation, and have used the predicted thermal and subsidence history of stretched basins to estimate the six reaction constants. Two of the reactions are isomerization reactions, at C-20 in a sterane and at C-22 in a hopane hydrocarbon. The third reaction converts C-ring monoaromatic to triaromatic steroid hydrocarbons. No single measure of maturity can describe the progress of these reactions. In old basins, such as the North Sea, both isomerization reactions are almost complete before appreciable aromatization has occurred, whereas in young basins, such as the Pannonian Basin in Hungary, aromatization is almost complete before appreciable isomerization of the steranes has occurred. We show that the calculated progress of these reactions agrees well with that observed in both basins if the frequency factors and activation energies are 6 x 10-3 s-1 and 91 kJ mol-1, 0.016 s-1 and 91 kJ mol-1, 1.8 x 1024 s-1 and 200 kJ mol-1 for the isomerization of steranes, of hopanes, and the aromatization of steroid hydrocarbons respectively. The rate of conversion of the R to the S form was taken to be 1.174 and 1.564 times that of the reverse reactions for sterane and hopane isomerizations respectively, and the aromatization reaction was assumed to be irreversible. All three reactions were assumed to be first order and unimolecular. The aromatization rate is consistent with laboratory observations. The rate of hopane isomerization is not, and different reaction mechanisms probably dominate at different temperatures. The same constants can be used to predict the progress of the reactions in basins which have been uplifted by inversion, such as the Lower Saxony Basin in West Germany. The geochemical observations provide estimates of the amount and time of uplift which agree with those from geological studies. Geochemical observations from the eastern part of the Paris Basin suggest that this region has also been uplifted by between 1 and 2 km.

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