Results 211 to 220 of about 389,431 (321)
The article demonstrates that brine was central for the supply of Ca and B to the studied saline lake. The ion transport occurred probably by thermal springs, while contributions from surface waters cannot be excluded. However, the saturation and syndepositional precipitation of Ca borates were initiated by an arid climate through evaporation, while ...
Nevena Andrić‐Tomašević+8 more
wiley +1 more source
Seismic evidence of liquid water at the base of Mars' upper crust. [PDF]
Sun W, Tkalčić H, Malusà MG, Pan Y.
europepmc +1 more source
Lacustrine Terraces and Crustal Movement around Lake Kucharo, Hokkaido
Shoji HORIE
openalex +2 more sources
RELATIVE HUMIDITY OVER A SNOW CRUST AND THE TRANSPIRATION OF CONIFERS [PDF]
Henry I. Baldwin
openalex +1 more source
Halite thickness in Mbr 2 of the Kumugeliemu can reach 1000 m. The thick halite is associated with sedimentary rock with shallow water fabrics. The thick halite was formed in a shallow‐sea water environment. The ‘Multiple transgression‐salt‐forming’ model was established.
Peng Qin, Dakang Zhong, Zhonggui Hu
wiley +1 more source
The importance of carbonatite lavas in outgassing Venus' modern-day atmosphere. [PDF]
Trussell AR+5 more
europepmc +1 more source
On the Determination of Crustal Structure by the Dispersion Curves of Surface Waves (II)
Ry ocirc suke SAT Ocirc
openalex +2 more sources
The Bisperode section is one of the most expanded and complete sections with shallow‐marine Oxfordian strata in the LSB. This study provides a reference record for shallow‐marine settings and allows for the correlation of the strata from the LSB with Oxfordian deposits distributed elsewhere in the world.
Deyan Zhang+3 more
wiley +1 more source
Exploring postoperative nasal airflow dynamics and impact on crust formation and mucosal healing after endoscopic tumor resection using computational fluid dynamics analysis. [PDF]
Na Y, Park M, Jung YG.
europepmc +1 more source
Bermuda patch reefs development was primarily controlled by massive coral framework construction, and variation in environmental energy, turbidity and bioerosion. These factors shaped the size, diversity and preservation of the framework, leading to a suppressed, steady vertical accretion.
Eduardo Islas‐Dominguez+2 more
wiley +1 more source