Results 61 to 70 of about 4,235 (222)
A palaeomagnetic study of Syrian volcanic rocks of Miocene to Holocene age [PDF]
Miocene and younger volcanic rocks from Syria show both normal and reversed polarities after thermal demagnetisation. Similarities in site mean directions may be used to establish lavas erupted at similar times.
A. L. Abdeldayem +3 more
doaj
Magnetostratigraphy of the Baynunah Formation
The Baynunah Formation in the Al Gharbia region of Abu Dhabi Emirate was deposited by a major fluvial system and preserves the only known late Miocene terrestrial fossils in the Arabian Peninsula. We analyzed paleomagnetic samples from six sections (Jebel Barakah, Shuwaihat 2, Hamra 5, Mleisa 1, Mleisa 2, and Kihal 2) to develop a polarity stratigraphy
Daniel J. Peppe +4 more
openaire +2 more sources
(Table S7) Magnetostratigraphy of Site 208-1262
(Table S7) Magnetostratigraphy of Site 208 ...
Simonetta Monechi (6886928) +15 more
core +1 more source
Abstract Intracontinental deformation records how early Eocene India–Asia collisional stress propagated into continental interiors. How rapidly compression reached the far field, and whether coeval Paleo‐Pacific slab dynamics contributed, remain debated. The Longzhong Basin, ∼1,900 km north of the collisional zone, provides a key test.
Zhantao Feng +8 more
wiley +1 more source
Objective The West Kunlun Orogenic Belt, located on the northwestern margin of the Tibetan Plateau, is a key area for studying the tectonic uplift and expansion of the plateau.
ZHANG Lijuan +4 more
doaj +1 more source
Integrated stratigraphy of the Upper Barremian–Aptian sediments from the south-eastern Crimea
Previous studies made in different parts of the world have shown that Barremian–Aptian times imply many difficulties in deciphering the biostratigraphy, microfossil evolution and correlation of bioevents.
Karpuk Maria S. +6 more
doaj +1 more source
Table S26 - Magnetostratigraphy ODP Site 208-1262
Table S26 - Magnetostratigraphy ODP Site 208 ...
James C Zachos (6958619) +13 more
core +1 more source
Table S28 - Magnetostratigraphy ODP Site 208-1265
Table S28 - Magnetostratigraphy ODP Site 208 ...
James C Zachos (6958619) +13 more
core +1 more source
Abstract Instantaneous event deposits such as turbidites, debrites, and slumps are common and frequently occur in marginal seas. These instantaneous deposits represent seconds to days in duration, and can therefore significantly impact age‐depth models and interpretation of paleoclimate history based on thick sedimentary sequences recovered in deep ...
Xunpeng Li +8 more
wiley +1 more source
In order to obtain the missing data on the magnetostratigraphy of transitional layers between Sarmatian and the Maeotian parts in the Eastern Paratethys, the authors studied the Upper Sarmatian ― the Lower Maeotian deposits in the Panagia Cape section ...
Pilipenko O.V. +4 more
doaj +1 more source

