Kaolins in gravels and saprolites in north-east Scotland: Evidence from stable H and O isotopes for Palaeocene–Miocene deep weathering
Stable isotope ratios can provide important evidence for estimating groundwater temperatures during the formation of clay minerals in response to chemical weathering of rocks at the landsurface. In this paper, we investigate weathering kaolins found in Buchan, NE Scotland. Stable oxygen and hydrogen...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Hall, Adrian M. [verfasserIn] |
|---|
| Format: |
E-Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2015transfer abstract |
|---|
| Umfang: |
11 |
|---|
| Übergeordnetes Werk: |
Enthalten in: The head constituent plays a key role in the lexical boost in syntactic priming - Huang, Jian ELSEVIER, 2023, Amsterdam [u.a.] |
|---|---|
| Übergeordnetes Werk: |
volume:424 ; year:2015 ; day:15 ; month:04 ; pages:6-16 ; extent:11 |
| Links: |
|---|
| DOI / URN: |
10.1016/j.palaeo.2015.02.019 |
|---|
| Katalog-ID: |
ELV029390397 |
|---|
| LEADER | 01000caa a22002652 4500 | ||
|---|---|---|---|
| 001 | ELV029390397 | ||
| 003 | DE-627 | ||
| 005 | 20230625172933.0 | ||
| 007 | cr uuu---uuuuu | ||
| 008 | 180603s2015 xx |||||o 00| ||eng c | ||
| 024 | 7 | |a 10.1016/j.palaeo.2015.02.019 |2 doi | |
| 028 | 5 | 2 | |a GBVA2015023000017.pica |
| 035 | |a (DE-627)ELV029390397 | ||
| 035 | |a (ELSEVIER)S0031-0182(15)00075-9 | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 041 | |a eng | ||
| 082 | 0 | |a 550 |a 930 | |
| 082 | 0 | 4 | |a 550 |q DE-600 |
| 082 | 0 | 4 | |a 930 |q DE-600 |
| 082 | 0 | 4 | |a 400 |a 370 |a 150 |q VZ |
| 084 | |a 5,3 |2 ssgn | ||
| 084 | |a LING |q DE-30 |2 fid | ||
| 084 | |a 17.00 |2 bkl | ||
| 100 | 1 | |a Hall, Adrian M. |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Kaolins in gravels and saprolites in north-east Scotland: Evidence from stable H and O isotopes for Palaeocene–Miocene deep weathering |
| 264 | 1 | |c 2015transfer abstract | |
| 300 | |a 11 | ||
| 336 | |a nicht spezifiziert |b zzz |2 rdacontent | ||
| 337 | |a nicht spezifiziert |b z |2 rdamedia | ||
| 338 | |a nicht spezifiziert |b zu |2 rdacarrier | ||
| 520 | |a Stable isotope ratios can provide important evidence for estimating groundwater temperatures during the formation of clay minerals in response to chemical weathering of rocks at the landsurface. In this paper, we investigate weathering kaolins found in Buchan, NE Scotland. Stable oxygen and hydrogen isotopes for kaolins from weathered clasts in post-Cretaceous fluvial gravels and from clay-rich saprolites developed in Dalradian metamorphic and Caledonian igneous rocks indicate weathering under warm groundwater temperatures of 23±5°C. Comparisons with Cenozoic palaeotemperatures derived from North Sea sediments indicate that weathering took place under humid tropical climates of the Palaeocene–Eocene. The >25m deep weathering profiles in the Buchan Gravels indicate that these coarse, quartzite- and flint-bearing gravels are older than previously thought and were likely deposited by rivers which also fed thick Palaeocene–Early Eocene deep-water sand fans in the western North Sea basin. A later phase of kaolin weathering at lower temperatures of 15±5°C took place in the Middle Miocene. Kaolinitic weathering remnants are largely confined to elevations of >100m in eastern Buchan and define a well-preserved, deeply weathered Cenozoic landscape in north-east Scotland. | ||
| 520 | |a Stable isotope ratios can provide important evidence for estimating groundwater temperatures during the formation of clay minerals in response to chemical weathering of rocks at the landsurface. In this paper, we investigate weathering kaolins found in Buchan, NE Scotland. Stable oxygen and hydrogen isotopes for kaolins from weathered clasts in post-Cretaceous fluvial gravels and from clay-rich saprolites developed in Dalradian metamorphic and Caledonian igneous rocks indicate weathering under warm groundwater temperatures of 23±5°C. Comparisons with Cenozoic palaeotemperatures derived from North Sea sediments indicate that weathering took place under humid tropical climates of the Palaeocene–Eocene. The >25m deep weathering profiles in the Buchan Gravels indicate that these coarse, quartzite- and flint-bearing gravels are older than previously thought and were likely deposited by rivers which also fed thick Palaeocene–Early Eocene deep-water sand fans in the western North Sea basin. A later phase of kaolin weathering at lower temperatures of 15±5°C took place in the Middle Miocene. Kaolinitic weathering remnants are largely confined to elevations of >100m in eastern Buchan and define a well-preserved, deeply weathered Cenozoic landscape in north-east Scotland. | ||
| 700 | 1 | |a Gilg, H. Albert |4 oth | |
| 700 | 1 | |a Fallick, Anthony E. |4 oth | |
| 700 | 1 | |a Merritt, Jon W. |4 oth | |
| 773 | 0 | 8 | |i Enthalten in |n Elsevier Science |a Huang, Jian ELSEVIER |t The head constituent plays a key role in the lexical boost in syntactic priming |d 2023 |g Amsterdam [u.a.] |w (DE-627)ELV010243836 |
| 773 | 1 | 8 | |g volume:424 |g year:2015 |g day:15 |g month:04 |g pages:6-16 |g extent:11 |
| 856 | 4 | 0 | |u https://doi.org/10.1016/j.palaeo.2015.02.019 |3 Volltext |
| 912 | |a GBV_USEFLAG_U | ||
| 912 | |a GBV_ELV | ||
| 912 | |a SYSFLAG_U | ||
| 912 | |a FID-LING | ||
| 912 | |a SSG-OPC-ANG | ||
| 936 | b | k | |a 17.00 |j Sprach- und Literaturwissenschaft: Allgemeines |q VZ |
| 951 | |a AR | ||
| 952 | |d 424 |j 2015 |b 15 |c 0415 |h 6-16 |g 11 | ||
| 953 | |2 045F |a 550 | ||
| author_variant |
a m h am amh |
|---|---|
| matchkey_str |
halladrianmgilghalbertfallickanthonyemer:2015----:alnigaesnspoieinrhatctadvdnermtbeadiooefra |
| hierarchy_sort_str |
2015transfer abstract |
| bklnumber |
17.00 |
| publishDate |
2015 |
| allfields |
10.1016/j.palaeo.2015.02.019 doi GBVA2015023000017.pica (DE-627)ELV029390397 (ELSEVIER)S0031-0182(15)00075-9 DE-627 ger DE-627 rakwb eng 550 930 550 DE-600 930 DE-600 400 370 150 VZ 5,3 ssgn LING DE-30 fid 17.00 bkl Hall, Adrian M. verfasserin aut Kaolins in gravels and saprolites in north-east Scotland: Evidence from stable H and O isotopes for Palaeocene–Miocene deep weathering 2015transfer abstract 11 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Stable isotope ratios can provide important evidence for estimating groundwater temperatures during the formation of clay minerals in response to chemical weathering of rocks at the landsurface. In this paper, we investigate weathering kaolins found in Buchan, NE Scotland. Stable oxygen and hydrogen isotopes for kaolins from weathered clasts in post-Cretaceous fluvial gravels and from clay-rich saprolites developed in Dalradian metamorphic and Caledonian igneous rocks indicate weathering under warm groundwater temperatures of 23±5°C. Comparisons with Cenozoic palaeotemperatures derived from North Sea sediments indicate that weathering took place under humid tropical climates of the Palaeocene–Eocene. The >25m deep weathering profiles in the Buchan Gravels indicate that these coarse, quartzite- and flint-bearing gravels are older than previously thought and were likely deposited by rivers which also fed thick Palaeocene–Early Eocene deep-water sand fans in the western North Sea basin. A later phase of kaolin weathering at lower temperatures of 15±5°C took place in the Middle Miocene. Kaolinitic weathering remnants are largely confined to elevations of >100m in eastern Buchan and define a well-preserved, deeply weathered Cenozoic landscape in north-east Scotland. Stable isotope ratios can provide important evidence for estimating groundwater temperatures during the formation of clay minerals in response to chemical weathering of rocks at the landsurface. In this paper, we investigate weathering kaolins found in Buchan, NE Scotland. Stable oxygen and hydrogen isotopes for kaolins from weathered clasts in post-Cretaceous fluvial gravels and from clay-rich saprolites developed in Dalradian metamorphic and Caledonian igneous rocks indicate weathering under warm groundwater temperatures of 23±5°C. Comparisons with Cenozoic palaeotemperatures derived from North Sea sediments indicate that weathering took place under humid tropical climates of the Palaeocene–Eocene. The >25m deep weathering profiles in the Buchan Gravels indicate that these coarse, quartzite- and flint-bearing gravels are older than previously thought and were likely deposited by rivers which also fed thick Palaeocene–Early Eocene deep-water sand fans in the western North Sea basin. A later phase of kaolin weathering at lower temperatures of 15±5°C took place in the Middle Miocene. Kaolinitic weathering remnants are largely confined to elevations of >100m in eastern Buchan and define a well-preserved, deeply weathered Cenozoic landscape in north-east Scotland. Gilg, H. Albert oth Fallick, Anthony E. oth Merritt, Jon W. oth Enthalten in Elsevier Science Huang, Jian ELSEVIER The head constituent plays a key role in the lexical boost in syntactic priming 2023 Amsterdam [u.a.] (DE-627)ELV010243836 volume:424 year:2015 day:15 month:04 pages:6-16 extent:11 https://doi.org/10.1016/j.palaeo.2015.02.019 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-LING SSG-OPC-ANG 17.00 Sprach- und Literaturwissenschaft: Allgemeines VZ AR 424 2015 15 0415 6-16 11 045F 550 |
| spelling |
10.1016/j.palaeo.2015.02.019 doi GBVA2015023000017.pica (DE-627)ELV029390397 (ELSEVIER)S0031-0182(15)00075-9 DE-627 ger DE-627 rakwb eng 550 930 550 DE-600 930 DE-600 400 370 150 VZ 5,3 ssgn LING DE-30 fid 17.00 bkl Hall, Adrian M. verfasserin aut Kaolins in gravels and saprolites in north-east Scotland: Evidence from stable H and O isotopes for Palaeocene–Miocene deep weathering 2015transfer abstract 11 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Stable isotope ratios can provide important evidence for estimating groundwater temperatures during the formation of clay minerals in response to chemical weathering of rocks at the landsurface. In this paper, we investigate weathering kaolins found in Buchan, NE Scotland. Stable oxygen and hydrogen isotopes for kaolins from weathered clasts in post-Cretaceous fluvial gravels and from clay-rich saprolites developed in Dalradian metamorphic and Caledonian igneous rocks indicate weathering under warm groundwater temperatures of 23±5°C. Comparisons with Cenozoic palaeotemperatures derived from North Sea sediments indicate that weathering took place under humid tropical climates of the Palaeocene–Eocene. The >25m deep weathering profiles in the Buchan Gravels indicate that these coarse, quartzite- and flint-bearing gravels are older than previously thought and were likely deposited by rivers which also fed thick Palaeocene–Early Eocene deep-water sand fans in the western North Sea basin. A later phase of kaolin weathering at lower temperatures of 15±5°C took place in the Middle Miocene. Kaolinitic weathering remnants are largely confined to elevations of >100m in eastern Buchan and define a well-preserved, deeply weathered Cenozoic landscape in north-east Scotland. Stable isotope ratios can provide important evidence for estimating groundwater temperatures during the formation of clay minerals in response to chemical weathering of rocks at the landsurface. In this paper, we investigate weathering kaolins found in Buchan, NE Scotland. Stable oxygen and hydrogen isotopes for kaolins from weathered clasts in post-Cretaceous fluvial gravels and from clay-rich saprolites developed in Dalradian metamorphic and Caledonian igneous rocks indicate weathering under warm groundwater temperatures of 23±5°C. Comparisons with Cenozoic palaeotemperatures derived from North Sea sediments indicate that weathering took place under humid tropical climates of the Palaeocene–Eocene. The >25m deep weathering profiles in the Buchan Gravels indicate that these coarse, quartzite- and flint-bearing gravels are older than previously thought and were likely deposited by rivers which also fed thick Palaeocene–Early Eocene deep-water sand fans in the western North Sea basin. A later phase of kaolin weathering at lower temperatures of 15±5°C took place in the Middle Miocene. Kaolinitic weathering remnants are largely confined to elevations of >100m in eastern Buchan and define a well-preserved, deeply weathered Cenozoic landscape in north-east Scotland. Gilg, H. Albert oth Fallick, Anthony E. oth Merritt, Jon W. oth Enthalten in Elsevier Science Huang, Jian ELSEVIER The head constituent plays a key role in the lexical boost in syntactic priming 2023 Amsterdam [u.a.] (DE-627)ELV010243836 volume:424 year:2015 day:15 month:04 pages:6-16 extent:11 https://doi.org/10.1016/j.palaeo.2015.02.019 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-LING SSG-OPC-ANG 17.00 Sprach- und Literaturwissenschaft: Allgemeines VZ AR 424 2015 15 0415 6-16 11 045F 550 |
| allfields_unstemmed |
10.1016/j.palaeo.2015.02.019 doi GBVA2015023000017.pica (DE-627)ELV029390397 (ELSEVIER)S0031-0182(15)00075-9 DE-627 ger DE-627 rakwb eng 550 930 550 DE-600 930 DE-600 400 370 150 VZ 5,3 ssgn LING DE-30 fid 17.00 bkl Hall, Adrian M. verfasserin aut Kaolins in gravels and saprolites in north-east Scotland: Evidence from stable H and O isotopes for Palaeocene–Miocene deep weathering 2015transfer abstract 11 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Stable isotope ratios can provide important evidence for estimating groundwater temperatures during the formation of clay minerals in response to chemical weathering of rocks at the landsurface. In this paper, we investigate weathering kaolins found in Buchan, NE Scotland. Stable oxygen and hydrogen isotopes for kaolins from weathered clasts in post-Cretaceous fluvial gravels and from clay-rich saprolites developed in Dalradian metamorphic and Caledonian igneous rocks indicate weathering under warm groundwater temperatures of 23±5°C. Comparisons with Cenozoic palaeotemperatures derived from North Sea sediments indicate that weathering took place under humid tropical climates of the Palaeocene–Eocene. The >25m deep weathering profiles in the Buchan Gravels indicate that these coarse, quartzite- and flint-bearing gravels are older than previously thought and were likely deposited by rivers which also fed thick Palaeocene–Early Eocene deep-water sand fans in the western North Sea basin. A later phase of kaolin weathering at lower temperatures of 15±5°C took place in the Middle Miocene. Kaolinitic weathering remnants are largely confined to elevations of >100m in eastern Buchan and define a well-preserved, deeply weathered Cenozoic landscape in north-east Scotland. Stable isotope ratios can provide important evidence for estimating groundwater temperatures during the formation of clay minerals in response to chemical weathering of rocks at the landsurface. In this paper, we investigate weathering kaolins found in Buchan, NE Scotland. Stable oxygen and hydrogen isotopes for kaolins from weathered clasts in post-Cretaceous fluvial gravels and from clay-rich saprolites developed in Dalradian metamorphic and Caledonian igneous rocks indicate weathering under warm groundwater temperatures of 23±5°C. Comparisons with Cenozoic palaeotemperatures derived from North Sea sediments indicate that weathering took place under humid tropical climates of the Palaeocene–Eocene. The >25m deep weathering profiles in the Buchan Gravels indicate that these coarse, quartzite- and flint-bearing gravels are older than previously thought and were likely deposited by rivers which also fed thick Palaeocene–Early Eocene deep-water sand fans in the western North Sea basin. A later phase of kaolin weathering at lower temperatures of 15±5°C took place in the Middle Miocene. Kaolinitic weathering remnants are largely confined to elevations of >100m in eastern Buchan and define a well-preserved, deeply weathered Cenozoic landscape in north-east Scotland. Gilg, H. Albert oth Fallick, Anthony E. oth Merritt, Jon W. oth Enthalten in Elsevier Science Huang, Jian ELSEVIER The head constituent plays a key role in the lexical boost in syntactic priming 2023 Amsterdam [u.a.] (DE-627)ELV010243836 volume:424 year:2015 day:15 month:04 pages:6-16 extent:11 https://doi.org/10.1016/j.palaeo.2015.02.019 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-LING SSG-OPC-ANG 17.00 Sprach- und Literaturwissenschaft: Allgemeines VZ AR 424 2015 15 0415 6-16 11 045F 550 |
| allfieldsGer |
10.1016/j.palaeo.2015.02.019 doi GBVA2015023000017.pica (DE-627)ELV029390397 (ELSEVIER)S0031-0182(15)00075-9 DE-627 ger DE-627 rakwb eng 550 930 550 DE-600 930 DE-600 400 370 150 VZ 5,3 ssgn LING DE-30 fid 17.00 bkl Hall, Adrian M. verfasserin aut Kaolins in gravels and saprolites in north-east Scotland: Evidence from stable H and O isotopes for Palaeocene–Miocene deep weathering 2015transfer abstract 11 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Stable isotope ratios can provide important evidence for estimating groundwater temperatures during the formation of clay minerals in response to chemical weathering of rocks at the landsurface. In this paper, we investigate weathering kaolins found in Buchan, NE Scotland. Stable oxygen and hydrogen isotopes for kaolins from weathered clasts in post-Cretaceous fluvial gravels and from clay-rich saprolites developed in Dalradian metamorphic and Caledonian igneous rocks indicate weathering under warm groundwater temperatures of 23±5°C. Comparisons with Cenozoic palaeotemperatures derived from North Sea sediments indicate that weathering took place under humid tropical climates of the Palaeocene–Eocene. The >25m deep weathering profiles in the Buchan Gravels indicate that these coarse, quartzite- and flint-bearing gravels are older than previously thought and were likely deposited by rivers which also fed thick Palaeocene–Early Eocene deep-water sand fans in the western North Sea basin. A later phase of kaolin weathering at lower temperatures of 15±5°C took place in the Middle Miocene. Kaolinitic weathering remnants are largely confined to elevations of >100m in eastern Buchan and define a well-preserved, deeply weathered Cenozoic landscape in north-east Scotland. Stable isotope ratios can provide important evidence for estimating groundwater temperatures during the formation of clay minerals in response to chemical weathering of rocks at the landsurface. In this paper, we investigate weathering kaolins found in Buchan, NE Scotland. Stable oxygen and hydrogen isotopes for kaolins from weathered clasts in post-Cretaceous fluvial gravels and from clay-rich saprolites developed in Dalradian metamorphic and Caledonian igneous rocks indicate weathering under warm groundwater temperatures of 23±5°C. Comparisons with Cenozoic palaeotemperatures derived from North Sea sediments indicate that weathering took place under humid tropical climates of the Palaeocene–Eocene. The >25m deep weathering profiles in the Buchan Gravels indicate that these coarse, quartzite- and flint-bearing gravels are older than previously thought and were likely deposited by rivers which also fed thick Palaeocene–Early Eocene deep-water sand fans in the western North Sea basin. A later phase of kaolin weathering at lower temperatures of 15±5°C took place in the Middle Miocene. Kaolinitic weathering remnants are largely confined to elevations of >100m in eastern Buchan and define a well-preserved, deeply weathered Cenozoic landscape in north-east Scotland. Gilg, H. Albert oth Fallick, Anthony E. oth Merritt, Jon W. oth Enthalten in Elsevier Science Huang, Jian ELSEVIER The head constituent plays a key role in the lexical boost in syntactic priming 2023 Amsterdam [u.a.] (DE-627)ELV010243836 volume:424 year:2015 day:15 month:04 pages:6-16 extent:11 https://doi.org/10.1016/j.palaeo.2015.02.019 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-LING SSG-OPC-ANG 17.00 Sprach- und Literaturwissenschaft: Allgemeines VZ AR 424 2015 15 0415 6-16 11 045F 550 |
| allfieldsSound |
10.1016/j.palaeo.2015.02.019 doi GBVA2015023000017.pica (DE-627)ELV029390397 (ELSEVIER)S0031-0182(15)00075-9 DE-627 ger DE-627 rakwb eng 550 930 550 DE-600 930 DE-600 400 370 150 VZ 5,3 ssgn LING DE-30 fid 17.00 bkl Hall, Adrian M. verfasserin aut Kaolins in gravels and saprolites in north-east Scotland: Evidence from stable H and O isotopes for Palaeocene–Miocene deep weathering 2015transfer abstract 11 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Stable isotope ratios can provide important evidence for estimating groundwater temperatures during the formation of clay minerals in response to chemical weathering of rocks at the landsurface. In this paper, we investigate weathering kaolins found in Buchan, NE Scotland. Stable oxygen and hydrogen isotopes for kaolins from weathered clasts in post-Cretaceous fluvial gravels and from clay-rich saprolites developed in Dalradian metamorphic and Caledonian igneous rocks indicate weathering under warm groundwater temperatures of 23±5°C. Comparisons with Cenozoic palaeotemperatures derived from North Sea sediments indicate that weathering took place under humid tropical climates of the Palaeocene–Eocene. The >25m deep weathering profiles in the Buchan Gravels indicate that these coarse, quartzite- and flint-bearing gravels are older than previously thought and were likely deposited by rivers which also fed thick Palaeocene–Early Eocene deep-water sand fans in the western North Sea basin. A later phase of kaolin weathering at lower temperatures of 15±5°C took place in the Middle Miocene. Kaolinitic weathering remnants are largely confined to elevations of >100m in eastern Buchan and define a well-preserved, deeply weathered Cenozoic landscape in north-east Scotland. Stable isotope ratios can provide important evidence for estimating groundwater temperatures during the formation of clay minerals in response to chemical weathering of rocks at the landsurface. In this paper, we investigate weathering kaolins found in Buchan, NE Scotland. Stable oxygen and hydrogen isotopes for kaolins from weathered clasts in post-Cretaceous fluvial gravels and from clay-rich saprolites developed in Dalradian metamorphic and Caledonian igneous rocks indicate weathering under warm groundwater temperatures of 23±5°C. Comparisons with Cenozoic palaeotemperatures derived from North Sea sediments indicate that weathering took place under humid tropical climates of the Palaeocene–Eocene. The >25m deep weathering profiles in the Buchan Gravels indicate that these coarse, quartzite- and flint-bearing gravels are older than previously thought and were likely deposited by rivers which also fed thick Palaeocene–Early Eocene deep-water sand fans in the western North Sea basin. A later phase of kaolin weathering at lower temperatures of 15±5°C took place in the Middle Miocene. Kaolinitic weathering remnants are largely confined to elevations of >100m in eastern Buchan and define a well-preserved, deeply weathered Cenozoic landscape in north-east Scotland. Gilg, H. Albert oth Fallick, Anthony E. oth Merritt, Jon W. oth Enthalten in Elsevier Science Huang, Jian ELSEVIER The head constituent plays a key role in the lexical boost in syntactic priming 2023 Amsterdam [u.a.] (DE-627)ELV010243836 volume:424 year:2015 day:15 month:04 pages:6-16 extent:11 https://doi.org/10.1016/j.palaeo.2015.02.019 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-LING SSG-OPC-ANG 17.00 Sprach- und Literaturwissenschaft: Allgemeines VZ AR 424 2015 15 0415 6-16 11 045F 550 |
| language |
English |
| source |
Enthalten in The head constituent plays a key role in the lexical boost in syntactic priming Amsterdam [u.a.] volume:424 year:2015 day:15 month:04 pages:6-16 extent:11 |
| sourceStr |
Enthalten in The head constituent plays a key role in the lexical boost in syntactic priming Amsterdam [u.a.] volume:424 year:2015 day:15 month:04 pages:6-16 extent:11 |
| format_phy_str_mv |
Article |
| bklname |
Sprach- und Literaturwissenschaft: Allgemeines |
| institution |
findex.gbv.de |
| dewey-raw |
550 |
| isfreeaccess_bool |
false |
| container_title |
The head constituent plays a key role in the lexical boost in syntactic priming |
| authorswithroles_txt_mv |
Hall, Adrian M. @@aut@@ Gilg, H. Albert @@oth@@ Fallick, Anthony E. @@oth@@ Merritt, Jon W. @@oth@@ |
| publishDateDaySort_date |
2015-01-15T00:00:00Z |
| hierarchy_top_id |
ELV010243836 |
| dewey-sort |
3550 |
| id |
ELV029390397 |
| language_de |
englisch |
| fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">ELV029390397</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230625172933.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">180603s2015 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1016/j.palaeo.2015.02.019</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">GBVA2015023000017.pica</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)ELV029390397</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ELSEVIER)S0031-0182(15)00075-9</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2=" "><subfield code="a">550</subfield><subfield code="a">930</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">DE-600</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">930</subfield><subfield code="q">DE-600</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">400</subfield><subfield code="a">370</subfield><subfield code="a">150</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">5,3</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">LING</subfield><subfield code="q">DE-30</subfield><subfield code="2">fid</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">17.00</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Hall, Adrian M.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Kaolins in gravels and saprolites in north-east Scotland: Evidence from stable H and O isotopes for Palaeocene–Miocene deep weathering</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2015transfer abstract</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">11</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">z</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zu</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Stable isotope ratios can provide important evidence for estimating groundwater temperatures during the formation of clay minerals in response to chemical weathering of rocks at the landsurface. In this paper, we investigate weathering kaolins found in Buchan, NE Scotland. Stable oxygen and hydrogen isotopes for kaolins from weathered clasts in post-Cretaceous fluvial gravels and from clay-rich saprolites developed in Dalradian metamorphic and Caledonian igneous rocks indicate weathering under warm groundwater temperatures of 23±5°C. Comparisons with Cenozoic palaeotemperatures derived from North Sea sediments indicate that weathering took place under humid tropical climates of the Palaeocene–Eocene. The >25m deep weathering profiles in the Buchan Gravels indicate that these coarse, quartzite- and flint-bearing gravels are older than previously thought and were likely deposited by rivers which also fed thick Palaeocene–Early Eocene deep-water sand fans in the western North Sea basin. A later phase of kaolin weathering at lower temperatures of 15±5°C took place in the Middle Miocene. Kaolinitic weathering remnants are largely confined to elevations of >100m in eastern Buchan and define a well-preserved, deeply weathered Cenozoic landscape in north-east Scotland.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Stable isotope ratios can provide important evidence for estimating groundwater temperatures during the formation of clay minerals in response to chemical weathering of rocks at the landsurface. In this paper, we investigate weathering kaolins found in Buchan, NE Scotland. Stable oxygen and hydrogen isotopes for kaolins from weathered clasts in post-Cretaceous fluvial gravels and from clay-rich saprolites developed in Dalradian metamorphic and Caledonian igneous rocks indicate weathering under warm groundwater temperatures of 23±5°C. Comparisons with Cenozoic palaeotemperatures derived from North Sea sediments indicate that weathering took place under humid tropical climates of the Palaeocene–Eocene. The >25m deep weathering profiles in the Buchan Gravels indicate that these coarse, quartzite- and flint-bearing gravels are older than previously thought and were likely deposited by rivers which also fed thick Palaeocene–Early Eocene deep-water sand fans in the western North Sea basin. A later phase of kaolin weathering at lower temperatures of 15±5°C took place in the Middle Miocene. Kaolinitic weathering remnants are largely confined to elevations of >100m in eastern Buchan and define a well-preserved, deeply weathered Cenozoic landscape in north-east Scotland.</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Gilg, H. Albert</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Fallick, Anthony E.</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Merritt, Jon W.</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="n">Elsevier Science</subfield><subfield code="a">Huang, Jian ELSEVIER</subfield><subfield code="t">The head constituent plays a key role in the lexical boost in syntactic priming</subfield><subfield code="d">2023</subfield><subfield code="g">Amsterdam [u.a.]</subfield><subfield code="w">(DE-627)ELV010243836</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:424</subfield><subfield code="g">year:2015</subfield><subfield code="g">day:15</subfield><subfield code="g">month:04</subfield><subfield code="g">pages:6-16</subfield><subfield code="g">extent:11</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1016/j.palaeo.2015.02.019</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ELV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">FID-LING</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-ANG</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">17.00</subfield><subfield code="j">Sprach- und Literaturwissenschaft: Allgemeines</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">424</subfield><subfield code="j">2015</subfield><subfield code="b">15</subfield><subfield code="c">0415</subfield><subfield code="h">6-16</subfield><subfield code="g">11</subfield></datafield><datafield tag="953" ind1=" " ind2=" "><subfield code="2">045F</subfield><subfield code="a">550</subfield></datafield></record></collection>
|
| author |
Hall, Adrian M. |
| spellingShingle |
Hall, Adrian M. ddc 550 ddc 930 ddc 400 ssgn 5,3 fid LING bkl 17.00 Kaolins in gravels and saprolites in north-east Scotland: Evidence from stable H and O isotopes for Palaeocene–Miocene deep weathering |
| authorStr |
Hall, Adrian M. |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)ELV010243836 |
| format |
electronic Article |
| dewey-ones |
550 - Earth sciences 930 - History of ancient world to ca. 499 400 - Language 370 - Education 150 - Psychology |
| delete_txt_mv |
keep |
| author_role |
aut |
| collection |
elsevier |
| remote_str |
true |
| illustrated |
Not Illustrated |
| topic_title |
550 930 550 DE-600 930 DE-600 400 370 150 VZ 5,3 ssgn LING DE-30 fid 17.00 bkl Kaolins in gravels and saprolites in north-east Scotland: Evidence from stable H and O isotopes for Palaeocene–Miocene deep weathering |
| topic |
ddc 550 ddc 930 ddc 400 ssgn 5,3 fid LING bkl 17.00 |
| topic_unstemmed |
ddc 550 ddc 930 ddc 400 ssgn 5,3 fid LING bkl 17.00 |
| topic_browse |
ddc 550 ddc 930 ddc 400 ssgn 5,3 fid LING bkl 17.00 |
| format_facet |
Elektronische Aufsätze Aufsätze Elektronische Ressource |
| format_main_str_mv |
Text Zeitschrift/Artikel |
| carriertype_str_mv |
zu |
| author2_variant |
h a g ha hag a e f ae aef j w m jw jwm |
| hierarchy_parent_title |
The head constituent plays a key role in the lexical boost in syntactic priming |
| hierarchy_parent_id |
ELV010243836 |
| dewey-tens |
550 - Earth sciences & geology 930 - History of ancient world (to ca. 499) 400 - Language 370 - Education 150 - Psychology |
| hierarchy_top_title |
The head constituent plays a key role in the lexical boost in syntactic priming |
| isfreeaccess_txt |
false |
| familylinks_str_mv |
(DE-627)ELV010243836 |
| title |
Kaolins in gravels and saprolites in north-east Scotland: Evidence from stable H and O isotopes for Palaeocene–Miocene deep weathering |
| ctrlnum |
(DE-627)ELV029390397 (ELSEVIER)S0031-0182(15)00075-9 |
| title_full |
Kaolins in gravels and saprolites in north-east Scotland: Evidence from stable H and O isotopes for Palaeocene–Miocene deep weathering |
| author_sort |
Hall, Adrian M. |
| journal |
The head constituent plays a key role in the lexical boost in syntactic priming |
| journalStr |
The head constituent plays a key role in the lexical boost in syntactic priming |
| lang_code |
eng |
| isOA_bool |
false |
| dewey-hundreds |
500 - Science 900 - History & geography 400 - Language 300 - Social sciences 100 - Philosophy & psychology |
| recordtype |
marc |
| publishDateSort |
2015 |
| contenttype_str_mv |
zzz |
| container_start_page |
6 |
| author_browse |
Hall, Adrian M. |
| container_volume |
424 |
| physical |
11 |
| class |
550 930 550 DE-600 930 DE-600 400 370 150 VZ 5,3 ssgn LING DE-30 fid 17.00 bkl |
| format_se |
Elektronische Aufsätze |
| author-letter |
Hall, Adrian M. |
| doi_str_mv |
10.1016/j.palaeo.2015.02.019 |
| dewey-full |
550 930 400 370 150 |
| title_sort |
kaolins in gravels and saprolites in north-east scotland: evidence from stable h and o isotopes for palaeocene–miocene deep weathering |
| title_auth |
Kaolins in gravels and saprolites in north-east Scotland: Evidence from stable H and O isotopes for Palaeocene–Miocene deep weathering |
| abstract |
Stable isotope ratios can provide important evidence for estimating groundwater temperatures during the formation of clay minerals in response to chemical weathering of rocks at the landsurface. In this paper, we investigate weathering kaolins found in Buchan, NE Scotland. Stable oxygen and hydrogen isotopes for kaolins from weathered clasts in post-Cretaceous fluvial gravels and from clay-rich saprolites developed in Dalradian metamorphic and Caledonian igneous rocks indicate weathering under warm groundwater temperatures of 23±5°C. Comparisons with Cenozoic palaeotemperatures derived from North Sea sediments indicate that weathering took place under humid tropical climates of the Palaeocene–Eocene. The >25m deep weathering profiles in the Buchan Gravels indicate that these coarse, quartzite- and flint-bearing gravels are older than previously thought and were likely deposited by rivers which also fed thick Palaeocene–Early Eocene deep-water sand fans in the western North Sea basin. A later phase of kaolin weathering at lower temperatures of 15±5°C took place in the Middle Miocene. Kaolinitic weathering remnants are largely confined to elevations of >100m in eastern Buchan and define a well-preserved, deeply weathered Cenozoic landscape in north-east Scotland. |
| abstractGer |
Stable isotope ratios can provide important evidence for estimating groundwater temperatures during the formation of clay minerals in response to chemical weathering of rocks at the landsurface. In this paper, we investigate weathering kaolins found in Buchan, NE Scotland. Stable oxygen and hydrogen isotopes for kaolins from weathered clasts in post-Cretaceous fluvial gravels and from clay-rich saprolites developed in Dalradian metamorphic and Caledonian igneous rocks indicate weathering under warm groundwater temperatures of 23±5°C. Comparisons with Cenozoic palaeotemperatures derived from North Sea sediments indicate that weathering took place under humid tropical climates of the Palaeocene–Eocene. The >25m deep weathering profiles in the Buchan Gravels indicate that these coarse, quartzite- and flint-bearing gravels are older than previously thought and were likely deposited by rivers which also fed thick Palaeocene–Early Eocene deep-water sand fans in the western North Sea basin. A later phase of kaolin weathering at lower temperatures of 15±5°C took place in the Middle Miocene. Kaolinitic weathering remnants are largely confined to elevations of >100m in eastern Buchan and define a well-preserved, deeply weathered Cenozoic landscape in north-east Scotland. |
| abstract_unstemmed |
Stable isotope ratios can provide important evidence for estimating groundwater temperatures during the formation of clay minerals in response to chemical weathering of rocks at the landsurface. In this paper, we investigate weathering kaolins found in Buchan, NE Scotland. Stable oxygen and hydrogen isotopes for kaolins from weathered clasts in post-Cretaceous fluvial gravels and from clay-rich saprolites developed in Dalradian metamorphic and Caledonian igneous rocks indicate weathering under warm groundwater temperatures of 23±5°C. Comparisons with Cenozoic palaeotemperatures derived from North Sea sediments indicate that weathering took place under humid tropical climates of the Palaeocene–Eocene. The >25m deep weathering profiles in the Buchan Gravels indicate that these coarse, quartzite- and flint-bearing gravels are older than previously thought and were likely deposited by rivers which also fed thick Palaeocene–Early Eocene deep-water sand fans in the western North Sea basin. A later phase of kaolin weathering at lower temperatures of 15±5°C took place in the Middle Miocene. Kaolinitic weathering remnants are largely confined to elevations of >100m in eastern Buchan and define a well-preserved, deeply weathered Cenozoic landscape in north-east Scotland. |
| collection_details |
GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-LING SSG-OPC-ANG |
| title_short |
Kaolins in gravels and saprolites in north-east Scotland: Evidence from stable H and O isotopes for Palaeocene–Miocene deep weathering |
| url |
https://doi.org/10.1016/j.palaeo.2015.02.019 |
| remote_bool |
true |
| author2 |
Gilg, H. Albert Fallick, Anthony E. Merritt, Jon W. |
| author2Str |
Gilg, H. Albert Fallick, Anthony E. Merritt, Jon W. |
| ppnlink |
ELV010243836 |
| mediatype_str_mv |
z |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| author2_role |
oth oth oth |
| doi_str |
10.1016/j.palaeo.2015.02.019 |
| up_date |
2024-07-06T21:20:12.971Z |
| _version_ |
1803866145262927872 |
| fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">ELV029390397</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230625172933.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">180603s2015 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1016/j.palaeo.2015.02.019</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">GBVA2015023000017.pica</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)ELV029390397</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ELSEVIER)S0031-0182(15)00075-9</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2=" "><subfield code="a">550</subfield><subfield code="a">930</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">DE-600</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">930</subfield><subfield code="q">DE-600</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">400</subfield><subfield code="a">370</subfield><subfield code="a">150</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">5,3</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">LING</subfield><subfield code="q">DE-30</subfield><subfield code="2">fid</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">17.00</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Hall, Adrian M.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Kaolins in gravels and saprolites in north-east Scotland: Evidence from stable H and O isotopes for Palaeocene–Miocene deep weathering</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2015transfer abstract</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">11</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">z</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zu</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Stable isotope ratios can provide important evidence for estimating groundwater temperatures during the formation of clay minerals in response to chemical weathering of rocks at the landsurface. In this paper, we investigate weathering kaolins found in Buchan, NE Scotland. Stable oxygen and hydrogen isotopes for kaolins from weathered clasts in post-Cretaceous fluvial gravels and from clay-rich saprolites developed in Dalradian metamorphic and Caledonian igneous rocks indicate weathering under warm groundwater temperatures of 23±5°C. Comparisons with Cenozoic palaeotemperatures derived from North Sea sediments indicate that weathering took place under humid tropical climates of the Palaeocene–Eocene. The >25m deep weathering profiles in the Buchan Gravels indicate that these coarse, quartzite- and flint-bearing gravels are older than previously thought and were likely deposited by rivers which also fed thick Palaeocene–Early Eocene deep-water sand fans in the western North Sea basin. A later phase of kaolin weathering at lower temperatures of 15±5°C took place in the Middle Miocene. Kaolinitic weathering remnants are largely confined to elevations of >100m in eastern Buchan and define a well-preserved, deeply weathered Cenozoic landscape in north-east Scotland.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Stable isotope ratios can provide important evidence for estimating groundwater temperatures during the formation of clay minerals in response to chemical weathering of rocks at the landsurface. In this paper, we investigate weathering kaolins found in Buchan, NE Scotland. Stable oxygen and hydrogen isotopes for kaolins from weathered clasts in post-Cretaceous fluvial gravels and from clay-rich saprolites developed in Dalradian metamorphic and Caledonian igneous rocks indicate weathering under warm groundwater temperatures of 23±5°C. Comparisons with Cenozoic palaeotemperatures derived from North Sea sediments indicate that weathering took place under humid tropical climates of the Palaeocene–Eocene. The >25m deep weathering profiles in the Buchan Gravels indicate that these coarse, quartzite- and flint-bearing gravels are older than previously thought and were likely deposited by rivers which also fed thick Palaeocene–Early Eocene deep-water sand fans in the western North Sea basin. A later phase of kaolin weathering at lower temperatures of 15±5°C took place in the Middle Miocene. Kaolinitic weathering remnants are largely confined to elevations of >100m in eastern Buchan and define a well-preserved, deeply weathered Cenozoic landscape in north-east Scotland.</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Gilg, H. Albert</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Fallick, Anthony E.</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Merritt, Jon W.</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="n">Elsevier Science</subfield><subfield code="a">Huang, Jian ELSEVIER</subfield><subfield code="t">The head constituent plays a key role in the lexical boost in syntactic priming</subfield><subfield code="d">2023</subfield><subfield code="g">Amsterdam [u.a.]</subfield><subfield code="w">(DE-627)ELV010243836</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:424</subfield><subfield code="g">year:2015</subfield><subfield code="g">day:15</subfield><subfield code="g">month:04</subfield><subfield code="g">pages:6-16</subfield><subfield code="g">extent:11</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1016/j.palaeo.2015.02.019</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ELV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">FID-LING</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-ANG</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">17.00</subfield><subfield code="j">Sprach- und Literaturwissenschaft: Allgemeines</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">424</subfield><subfield code="j">2015</subfield><subfield code="b">15</subfield><subfield code="c">0415</subfield><subfield code="h">6-16</subfield><subfield code="g">11</subfield></datafield><datafield tag="953" ind1=" " ind2=" "><subfield code="2">045F</subfield><subfield code="a">550</subfield></datafield></record></collection>
|
| score |
7.401087 |