Clay-Mineral Distribution in Recent Sediments from Northern Pacific Coast of Mexico: ABSTRACT

AAPG Bulletin ◽  
1966 ◽  
Vol 50 ◽  
Author(s):  
Jorge de la Torre, Arman F. Frederi
Keyword(s):  
Clay Mineral ◽  
Pacific Coast ◽  
Mineral Distribution ◽  
Northern Pacific ◽  
Recent Sediments

From Ranching to Fishing – The Cultural Landscape of the Northern Pacific Coast of Baja California, Mexico

2016 ◽  
Vol 59 ◽  
Author(s):  
Antoinette WinklerPrins ◽  
Pablo Alvarez ◽  
Gerardo Bocco ◽  
Ileana Espejel
Keyword(s):  
Cultural Landscape ◽  
Baja California ◽  
Pacific Coast ◽  
Northern Pacific

scholarly journals Mysidopsis gemina n. sp. (Crustacea: Mysida: Mysidae) from the northern Pacific coast of Costa Rica

Nauplius ◽  
2019 ◽  
Vol 27 ◽  
Author(s):  
W. Wayne Price ◽  
Richard W. Heard ◽  
Rita Vargas
Keyword(s):  
Costa Rica ◽  
Pacific Coast ◽  
Northern Pacific

Clay mineral distribution in the shelf sediments off the northern part of the east coast of India

1988 ◽  
Vol 8 (2) ◽  
pp. 145-151 ◽  
Author(s):  
V. Purnachandra Rao ◽  
N. Purnachander Reddy ◽  
Ch. Madhusudana Rao
Keyword(s):  
Clay Mineral ◽  
East Coast ◽  
Mineral Distribution ◽  
East Coast Of India ◽  
Shelf Sediments

Reservoir Quality Assessment from Clay Mineral Distribution in the Neogene of North Kuwait

2014 ◽  
Author(s):  
P. Kumar Mishra ◽  
B. Hussain Akbar ◽  
K. Ahmed ◽  
H. Ferdous ◽  
L. Javier ◽  
...  
Keyword(s):  
Quality Assessment ◽  
Clay Mineral ◽  
Reservoir Quality ◽  
Mineral Distribution

The Early Postclassic Aztatlán Colonization of the Pacific Coast of Jalisco

2020 ◽  
pp. 131-156
Author(s):  
Joseph B. Mountjoy ◽  
Fabio Germán Cupul-Magaña ◽  
Rafael García de Quevedo-Machain ◽  
Martha Lorenza López Mestas Camberos
Keyword(s):  
Pacific Coast ◽  
Archaeological Site ◽  
Postclassic Period ◽  
Subsistence Strategies ◽  
Specialized Production ◽  
The Pacific ◽  
West Mexico ◽  
Early Postclassic ◽  
Northern Pacific

The focus of this chapter is a recently discovered archaeological site, Arroyo Piedras Azules, located on the northern Pacific coast of Jalisco, Mexico. Excavated materials provide considerable information about the colonization of this area by Aztatlán groups in the Early Postclassic period, as well as the nature of the expansion of the Aztatlán phenomenon in West Mexico. Based on the data thus far obtained from the site, the authors offer five significant conclusions regarding the development and the spread of the Aztatlán archaeological culture in West Mexico, concerning the timing of development, subsistence strategies of Pacific coastal groups, the nature of Aztatlán expansion, specialized production, and links between the Arroyo Piedras Azules site to the Mixteca-Puebla area.

Controls on Clay Mineral Distribution and Chemistry in the Early Permian Rotliegend of Germany

Clay Minerals ◽  
1993 ◽  
Vol 28 (3) ◽  
pp. 393-416 ◽  
Author(s):  
J. D. Platt
Keyword(s):  
Isotopic Composition ◽  
Clay Minerals ◽  
Clay Mineral ◽  
Tectonic Activity ◽  
Early Permian ◽  
Permian Basin ◽  
Mineral Distribution ◽  
Coal Measures

AbstractAuthigenic clay minerals in the German Rotliegend formed mainly at burial depths >1.5 km. Illite is the dominant cement, although kaolinite, dickite and early radial chlorite are abundant locally. Illites contain more AI and late chlorites more AI and Fe in sequences showing extensive grain dissolution. This relationship between clay chemistry and grain dissolution suggests that clay cementation is linked to grain dissolution. Sequences at relatively shallow burial depths (<3-5 km) contain less clay cement. In the more deeply buried sections, increased illite and kandite cementation, together with extensive grain dissolution, is evident where the Rotliegend is juxtaposed against Carboniferous Coal Measures. Faults also acted as important conduits for acidic fluids. Illite and kandite growth occurred at similar depths and from waters of similar isotopic composition (618O = 1-6‰ SMOW) throughout most of the Southern Permian Basin. However, the timing of illite growth varied between areas and corresponded to periods to tectonic activity.

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