Results 21 to 30 of about 97,532 (300)

Petrochemical Characteristics of Cenozoic Basalts in Datong, Shanxi

Taiyuan Ligong Daxue xuebao, 2021
Basalt in the Cenozoic period in Datong, Shanxi can be divided into two types: alkaline basalt in the northwest and tholeiite basalt in the southeast. Petrological and geochemical analyses were carried out on the basalts in Datong area. As known from the
Xiaoqin LI, Xin NIE, Zhuona BAI, Hongfu LIU, Zhiqiang FENG   +4 more
doaj   +1 more source

The latest geodynamics in Central Asia: primary and secondary mantle melting anomalies in the context of orogenesis, rifting, and lithospheric plate motions and interactions

Геодинамика и тектонофизика, 2017
A comprehensive model for deep dynamics in Asia has been developed from the data on the evolution of melting anomalies in the context of lithospheric plate motions, interactions, orogeny, and rifting.
I. S. Chuvashova, S. V. Rasskazov, Sun Yi-min   +2 more
doaj   +1 more source

Reconstructing Cenozoic vegetation from proxy data and models – A NECLIME synthesis (Editorial) [PDF]

, 2017
[No abstract ...
Bruch, Angela A., François, Louis, Spicer, Robert A., Spicer, Teresa, Utescher, Torsten   +4 more
core   +1 more source

Paleoclimatic and provenance implications of magnetic parameters from the Miocene sediments in the Subei Basin

Earth and Planetary Physics, 2020
Thick sediments from foreland basins usually provide valuable information for understanding the relationships between mountain building, rock denudation, and sediment deposition.
YouSheng Li, JiMin Sun, ZhiLiang Zhang, Bai Su, ShengChen Tian, MengMeng Cao   +5 more
doaj   +1 more source

The karst and palaeokarst of North and North-East Greenland – physical records of cryptic geological intervals

GEUS Bulletin, 2022
Carbonate rocks of Neoproterozoic to Silurian age are abundantly distributed around the coasts of North and North-East Greenland. Palaeokarst horizons are particularly well developed within the Portfjeld Formation (Ediacaran – earliest Cambrian) and ...
M. Paul Smith, Gina E. Moseley
doaj   +1 more source

Cenozoic stratigraphic correlation and the lower limit of Quaternary in Guanzhong Basin

地质科技通报, 2021
Thick Cenozoic sediments in Guanzhong Basin provide excellent geological records for the study of the regional tectonics, sediment environment evolution and paleoclimate change.However, there are still controversies about the Cenozoic stratigraphic ...
Yougui Song, Minwen Lan, Huifang Liu, Maosheng Zhang, Xiaofen Fu, Qiangqiang Ning   +5 more
doaj   +1 more source

How local crustal properties influence the amount of denudation derived from low-temperature: Comment [PDF]

, 2018
No abstract ...
Westaway, Rob
core   +1 more source

The late Mesozoic-Cenozoic tectonic evolution of the South China Sea: A petrologic perspective [PDF]

, 2014
This paper presents a review of available petrological, geochonological and geochemical data for late Mesozoic to Recent igneous rocks in the South China Sea (SCS) and adjacent regions and a discussion of their petrogeneses and tectonic implications. The
Castillo, PR, Shi, X, Yan, Q
core   +2 more sources

Cementation scenarios for New Zealand Cenozoic nontropical limestones [PDF]

, 1996
Cenozoic limestones are widely distributed in New Zealand, especially in the Oligocene-earliest Miocene in both islands, and the Pliocene-Pleistocene in North Island.
Hood, Steven D., Nelson, Campbell S.
core   +2 more sources

History of oceanic front development in the New Zealand sector of the Southern Ocean during the Cenozoic--a synthesis [PDF]

, 2001
The New Zealand sector of the Southern Ocean (NZSSO) has opened about the Indian-Pacific spreading ridge throughout the Cenozoic. Today the NZSSO is characterised by broad zonal belts of antarctic (cold), subantarctic (cool), and subtropical (warm ...
Abelmann A., Abreu V. S., Arnold A. J., Baldauf J. G., Baldauf J. G., Barker P. F., Barrera E., Berggren W. A., Beu A. G., Chaproniere G. C. H., Crux J. A., Devereux I., Edwards A. R., Edwards A. R., Fordyce R. E., Gordon A. L., Hampton M. A., Hanna E., Harwood D. M., Head P. S., Hollis C. J., Hornibrook N. de B., Hornibrook N. de B., Jaques A. L., Jenkins D. G., Keany J., Keller G., Kennett D. M., Kennett J. P., Kennett J. P., Kennett J. P., Kennett J. P., Kennett J. P., Kennett J. P., Kennett J. P., Kennett J. P., Lawver L. A., Lawver L. A., Lazarus D., Mackie J., Miller K. G., Murphy M. G., Nelson C. S., O'Connell S. B., Pearce F., Raymo M., Rohling E. J., Sancetta C., Sancetta C., Shackleton N. J., Shackleton N. J., Shafik S., Stott L. D., Sutherland F. L., Tsuchi R., Van Couvering J. A., Vella P., Wei W., Wise S. W., Wolfe J. A., Zachos J. C.   +60 more
core   +4 more sources