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What controlled Mid–Late Miocene long-term aridification in Central Asia?—Global cooling or Tibetan Plateau uplift: A review
Y Miao, M Herrmann, F Wu, X Yan, S Yang - Earth-Science Reviews, 2012 - Elsevier
Debate continues over whether global cooling or uplift of the Tibetan Plateau provided the
first-order driver for the aridification (moisture levels) of Central Asia throughout the Mid …
first-order driver for the aridification (moisture levels) of Central Asia throughout the Mid …
The geologic history of plants and climate in India
India's diverse vegetation and landscapes provide an opportunity to understand the
responses of vegetation to climate change. By examining pollen and fossil records along …
responses of vegetation to climate change. By examining pollen and fossil records along …
Predominant floodplain over mountain weathering of Himalayan sediments (Ganga basin)
We present an extensive river sediment dataset covering the Ganga basin from the
Himalayan front downstream to the Ganga mainstream in Bangladesh. These sediments …
Himalayan front downstream to the Ganga mainstream in Bangladesh. These sediments …
Increasing chemical weathering in the Himalayan system since the Last Glacial Maximum
Continental chemical weathering is central in Earth's surface biogeochemical cycles as it
redistributes elements across reservoirs such as the crust and the oceans. However the …
redistributes elements across reservoirs such as the crust and the oceans. However the …
Pore fluid evolution, distribution and water-rock interactions of carbonate cements in red-bed sandstone reservoirs in the Dongying Depression, China
J Wang, Y Cao, K Liu, J Liu, X Xue, Q Xu - Marine and Petroleum Geology, 2016 - Elsevier
The compositions, distribution and its interaction with rocks of the evolving pore fluids
controls the distribution of carbonate cements and reservoir storage spaces. The reservoir …
controls the distribution of carbonate cements and reservoir storage spaces. The reservoir …
[HTML][HTML] Authigenic clay minerals and calcite dissolution influence reservoir quality in tight sandstones: Insights from the central Junggar Basin, NW China
D Hong, J Cao, T Wu, S Dang, W Hu, S Yao - Energy Geoscience, 2020 - Elsevier
Authigenic clays and calcite cements are important in the development of reservoir tightness
and the formation of hydrocarbon sweet spots. We investigated Jurassic low-permeability …
and the formation of hydrocarbon sweet spots. We investigated Jurassic low-permeability …
Intensification of monsoon, microclimate and asynchronous C4 appearance: isotopic evidence from the Indian Siwalik sediments
Analysis of the D/H ratio of pedogenic clay and the 18O/16O ratio of carbonate nodules
collected from Siwalik sediments in India indicates three episodes of monsoon …
collected from Siwalik sediments in India indicates three episodes of monsoon …
Diagenetic fluid evolution and water-rock interaction model of carbonate cements in sandstone: An example from the reservoir sandstone of the Fourth Member of the …
SB Liu, SJ Huang, ZM Shen, ZX Lü… - Science China Earth …, 2014 - Springer
Carbonate cement is the most abundant cement type in the Fourth Member of the Xujiahe
Formation in the **aoquan-Fenggu area of the West Sichuan Depression. Here we use a …
Formation in the **aoquan-Fenggu area of the West Sichuan Depression. Here we use a …
Leaf physiognomy records the Miocene intensification of the South Asia Monsoon
Our understanding regarding the onset and development of the modern South Asia
monsoon (SAM) is still incomplete due to its complex nature and differing views about its …
monsoon (SAM) is still incomplete due to its complex nature and differing views about its …
Petrology of Bengal Fan turbidites (IODP Expeditions 353 and 354): provenance versus diagenetic control
High-resolution petrographic and heavy-mineral analyses of Bengal Fan turbidites from six
cores drilled during IODP Expeditions 353 and 354 elucidate factors controlling their …
cores drilled during IODP Expeditions 353 and 354 elucidate factors controlling their …