Himalaya to the sea: geology, geomorphology and the quaternary
Gespeichert in:
Format: | Buch |
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Sprache: | English |
Veröffentlicht: |
London [u.a.]
Routledge
1993
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Ausgabe: | 1. publ. |
Schlagworte: | |
Online-Zugang: | Inhaltsverzeichnis |
Beschreibung: | XXVII, 429 S. Ill., graph. Darst., Kt. |
ISBN: | 0415066484 |
Internformat
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245 | 1 | 0 | |a Himalaya to the sea |b geology, geomorphology and the quaternary |c ed. by John F. Shroder |
250 | |a 1. publ. | ||
264 | 1 | |a London [u.a.] |b Routledge |c 1993 | |
300 | |a XXVII, 429 S. |b Ill., graph. Darst., Kt. | ||
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650 | 4 | |a Geology |z Himalaya Mountains Region | |
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650 | 4 | |a Geology, Stratigraphic |y Neogene | |
650 | 4 | |a Geology, Stratigraphic |y Quaternary | |
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adam_text | HIMALAYA TO THE SEA
Geology, geomorphology and the Quaternary
Edited by
John F Shroder, jr
§
London and New York
CONTENTS
List of plates ix
List of figures xi
List of tables xvii
List of contributors xviii
Foreword xx
Preface xxiii
Acknowledgements xxvi
1 HIMALAYA TO THE SEA: GEOMORPHOLOGY AND
THE QUATERNARY OF PAKISTAN IN THE REGIONAL
CONTEXT 1
John F Shroder, jr
2 MIOCENE TO HOLOCENE UPLIFT AND SEDIMENTATION
IN THE NORTHERN HIMALAYA AND ADJACENT AREAS 43
Michael E Brookfield
3 PRESENT AND PAST PATTERNS OF GLACIATION IN
THE NORTHWEST HIMALAYA: CLIMATIC, TECTONIC
AND TOPOGRAPHIC CONTROLS 72
Jonathan A Holmes
4 REVISED CHRONOSTRATIGRAPHY OF THE LATE
CENOZO1C BUNTHANG SEQUENCE OF SKARDU
INTERMONTANE BASIN, KARAKORAM HIMALAYA,
PAKISTAN 91
Vincent S Cronin and Gary D Johnson
5 QUATERNARY AND HOLOCENE INTERMONTANE
BASIN SEDIMENTATION IN THE KARAKORAM
MOUNTAINS 108
Lewis A Owen and Edward Derbyshire
6 QUATERNARY GLACIATION OF THE KARAKORAM
AND NANGA PARBAT HIMALAYA 132
John F Shroder, jr , Lewis Owen and Edward Derbyshire
vii
CONTENTS
7 ALTITUDINAL ORGANIZATION OF KARAKORAM
GEOMORPHIC PROCESSES AND DEPOSITIONAL
ENVIRONMENTS 159
Kenneth Hewitt
8 SEDIMENT TRANSPORT AND YIELD AT THE RAIKOT
GLACIER, NANGA PARBAT, PUNJAB HIMALAYA 184
James S Gardner and Norman K Jones
9 POSITION OF THE PALAEOINDUS AS REVEALED BY THE
MAGNETIC STRATIGRAPHY OF THE SHINGHAR AND
SURGHAR RANGES, PAKISTAN 198
M Javed Khan and Neil D Opdyke
10 PALAEOECOLOGIC RECONSTRUCTION OF
FLOODPLAIN ENVIRONMENTS USING PALAEOSOLS
FROM UPPER SIWAL1K GROUP SEDIMENTS, NORTHERN
PAKISTAN 213
Jay Quade, Thure E Ceding, John R Bowman and M Asifjah
11 THE PALAEOCLIM AT1C SIGNIFICANCE OF THE LOESS
DEPOSITS IN NORTHERN PAKISTAN 227
H M Rendell
12 DECREASED TECTONISM OF THE SUI DOME 236
D Papastamatiou and C Vita-Finzi
13 SURFACE SOILS AND INDUS RIVER SEDIMENTS 251
Mirza Arshad AH Beg
14 FLUVIAL GEOMORPHOLOGY OF THE LOWER INDUS
BASIN (SINDH, PAKISTAN) AND THE INDUS
CIVILIZATION 265
Louis Flam
15 MORPHOLOGY AND DYNAMICS OF THE INDUS RIVER:
IMPLICATIONS FOR THE MOHEN JO DARO SITE 288
David W Jorgensen, Michael D Harvey, S A Schumm
and Louis Flam
16 UPLIFTED MARINE TERRACES ALONG THE MAKRAN
COAST OF PAKISTAN AND IRAN 327
Rodman J Snead
17 GEOGRAPHY, GEOMORPHIC PROCESS AND EFFECTS
ON ARCHAEOLOGICAL SITES ON THE MAKRAN COAST 363
Rodman J Snead
References 379
Index 411
viii
PLATES
51A major neotectonic thrust in the middle Indus valley
nearLichar 112
5 2 Oblique lateral view of the Ghulkin glacier in the upper
Hunza valley 118
5 3 View of the snout of the Pasu glacier and its proglacial lake
from hummocky moraines in the upper Hunza valley 119
5 4 Large debris cones in the Bagrot valley 122
5 5 Terraces comprised of lacustrine silts at Serat in the middle
Hunza valley 126
5 6 View of alluvial fans in the Gilgit valley near Jutial (10 km
southeast of Gilgit) 127
6 1 Jalipur alluvial facies sandstone dipping unbroken NW 60°
for 150 m into the Indus river below 141
6 2 The Ke Ges syncline with steeply dipping Jalipur till or tillite
forming the steep cliff across the Indus river 144
7 1 View down Barpu glacier from the ridge between Miar and
Sumaiyar Bar tributaries 171
7 2 The glacier margins in Zone III from above the terminus of
Barpu glacier 175
7 3 The ice-margin depression and base of slope deposits at
~ 3500 m altitude along the Barpu glacier 177
7 4 View across the ice-margin depression and base of slope
deposits at ~ 4085 m altitude on the left flank of
Biafo glacier 178
7 5 The depositional apron in altitude Zone II (5000-5300 m
altitude) along the margins of Golden Peak tributary,
Barpu glacier 179
8 1 The terminus and lower portion of the Raikot glacier in July
1986 with the north face of Nanga Parbat in the
background 187
8 2 The upper ablation zone, icefalls and part of the accumulation
area of the Raikot glacier 189
LIST OF PLATES
8 3 Basal conditions at the Raikot glacier as exposed within the
meltwater stream portal 193
12 1 Landsat mosaic of the region 237
12 2 View northward from Site 3 showing structural benches
developed by relatively resistant strata 241
12 3 Fill terrace and bench produced by hard bed in Asreli valley
(Site 5) 242
12 4 Normal fault in lower Siwaliks near Site 1 243
12 5 Slickensides in probable fault gouge near Site 1 244
12 6 Strike-slip fault in lower Siwalik sands at Site 14 245
12 7 Vertically displaced cemented gravels in lower Siwaliks
produced either by normal faulting or more probably by
block collapse after undercutting by wadi flow 246
12 8 Pipe leading to enlarged joint in bank of ravine 247
12 9 Discontinuous stepped gully developed from partially
collapsed pipe 248
12 10 Close-up of partially collapsed pipe of Plate 12 9 249
16 1 Cross-section of the uplifted Tis terrace in Iran showing
sharp unconformity between the Pleistocene conglomerates
and shelly limestones that cap the tilted Talar sandstones of
Oligocene-Miocene age 344
16 2 Slickensides indicating faulting which is so common along
the Makran coast 345
16 3 Holocene marine oyster shells imbedded in the surface
conglomerates of the Gwadar terrace in Pakistan, 90 m
above mean sea level 347
16 4 Paired stream terraces ~ 50 km inland from Chah Bahar,
Iran, on the road to Zahedan 350
16 5 The Konarak platform, which is one of the more prominent
terraces occurring along the Makran coast of Iran 354
16 6 The well developed Chah Bahar terrace in Iran 354
16 7 Wave-cut sea arch along Hawks Bay ~ 30 km east of
Cape Monze, Pakistan 355
16 8 Steeply dipping wave-cut platform on the west side of Hawks
Bay near the eastern flanks of Cape Monze in the eastern
section of the Pakistani coastal terraces 355
16 9 Wave-cut terraces and platforms along the Nishar section of
the Iran Makran coast 358
FIGURES
1 1 Index map of Pakistan, Afghanistan and part of northwest
India 2
1 2 The various mountain ranges of the western Himalaya
are part of a single geologic complex formed after the
collision of the Indo-Pakistani and the Eurasian crustal
plates 4
1 3 Schematic diagram of the course of the Indus river between
Haramosh and Nanga Parbat mountains and beside the
Raikot fault trace 8
1 4 Schematic diagram of two possible hypotheses for deflection
of the Indus river across the Nanga Parbat syntaxial bending
or offset of faults 9
1 5 Map of the western Himalaya showing a few of the larger
glaciers and slope failures studied, as well as other features
mentioned in the text 11
1 6 Terminus of Batura glacier in 1991 showing changes since
1 7 Sketch map of slope failures that partially or fully blocked
the Indus river 22
1 8 Generalized landforms of Pakistan with soil parent
materials 25
1 9 Reconstruction of the past drainage net across the Punjab 27
1 10 Generalized map of sand ridge landforms in the Thai desert
interfluvial area between the Indus river and the Jhelum and
Chenab rivers 35
1 11 Distribution and morphology of aeolian sand in the Thar
desert of India and Pakistan 36
1 12 Map of the lower Indus plain showing outline of presumed
late Pleistocene entrenched channel of the Indus 38
2 1 Location map for the northwestern Himalaya syntaxis and
adjacent areas 46
xi
LIST OF FIGURES
2 2 Rates of subsidence (really sedimentation rates) in the Tadzhik
basin 49
2 3 Uplift of the Pamir in the last 3 myr 50
2 4 Location map of Himalayan intermontane and piggyback
basins 53
2 5 Cooling curves for various tectonic units of Figure 2 1 55
2 6 Sedimentary budgets for Oligocene (A) and early to
mid-Miocene (B) 64
2 7 Sediment budgets for the late Miocene to Holocene 65
2 8 Diagram showing method of calculating width of block
removed by erosion at different periods 67
2 9 A: uncorrected altitudes from floras and faunas for the
Himalaya and southern Tibet; B: altitudes of the Tibet
plateau based on floras and faunas 69
2 10 River gradients and Himalayan biogeographic boundaries 70
3 1 Northwest Himalaya, showing the location of meterological
stations and other sites mentioned in the text 73
3 2 Isoglacihypses of (a) the equilibrium-line altitude; (b) the
glaciation threshold; and (c) cirque altitudes in Kashmir 82
3 3 Cross-section of Kashmir basin, showing the height of the
glaciation threshold and cirque altitudes 85
4 1 Location maps showing the distribution of several major
intermontane basins within the structural framework of the
northwest Himalaya, northern Pakistan and India 93
4 2 Schematic cross-section of the Bunthang outcrop on the
northeast side of Skardu valley 96
4 3 Schematic stratigraphic column through the middle
Bunthang sequence, as it is exposed on the northwest side
of Bunthang in Ghothamal canyon, above Komara 99
4 4 Zijderveld projections of the thermal demagnetization of
representative samples from each of the four newly sampled
sites 102
4 5 Equal-area stereonet displaying site mean values for all 76
class I and II sites in the Bunthang sequence 104
4 6 Comparison of the MPS of the Bunthang sequence with the
magnetic polarity time scale 105
5 1 Topographic and drainage map of the Karakoram
mountains, western Himalaya and adjacent foreland basins
showing the major geological structures 111
5 2 Schematic diagram showing the environmental and
geomorphological settings with the main landform types
in the Karakoram mountains 115
5 3 Main landforms and lithofacies associated with a Ghulkin
type glacier 116
xii
LIST OF FIGURES
5 4 Main landforms associated with a Pasu type glacier 120
5 5 The main types of mass movement processes and
landforms in the Karakoram mountains 123
5 6 Schematic diagram showing the main sources, movement
and deposition of silts in the Karakoram mountains 124
5 7 Diagram showing the interaction between the main
environmental systems that contributed to the evolution of
the Karakoram landscape 130
6 1 Index map of the study area 134
6 2 Index map of the type section area of the Jalipur formation
outcrops 142
6 3 Overturned syncline in Jalipur sediments at Patro near
Jalipur village along trace of the Raikot fault 145
7 1 The Karakoram range and its location in southwest
Central Asia, showing the extent of perennial snow and ice,
and the major river systems 160
7 2 General hypsometric curve for the upper Indus basin above
the Tarbela Dam, showing approximate altitudes of
precipitation zones 162
7 3 Schematic diagram showing the altitudinal distribution of
environmental variables, in relation to prevalent geomorphic
processes in the central Karakoram 163
7 4 Area-altitude distributions of the glacierized and off-ice
surfaces of the Barpu-Bualtar and Biafo glacier basins,
central Karakoram 164
7 5 Seasonal migration of temperature zones for the Karakoram
range, emphasizing zones of continuous freezing, of above freezing
temperatures and of frequent diurnal freeze-thaw cycles 166
7 6 Topographic map of the Biafo basin showing the location
and extent of the depositional landform complex along the
ablation-zone margins 173
7 7 Topographic map of the Barpu-Bualtar basin showing the
location and extent of the depositional landform complex
along the ablation-zone margins 174
8 1 The study area location and the Raikot (Rakhiot) glacier 185
8 2 The longitudinal surface profile of the Raikot glacier and the
hypsometric (area-altitude) distribution for the glacier-covered area 188
9 1 Geologic sketch-map of northern Pakistan 199
9 2 Geologic map of the Trans-Indus Salt range, northwestern
Pakistan 201
9 3 An example of partial thermal demagnetization: orthogonal
diagrams (Zijderveld diagrams) based on successive end
points of partial thermal demagnetization vectors 203
9 4 Equal-angle stereographic projections of bedding-corrected
xiii
LIST OF FIGURES
site-mean directions obtained after thermal demagnetization
at 500 °C and 600 °C 204
9 5 Plot of VGP latitude against stratigraphic thickness at
Spalmai Tangi 205
9 6 Plot of VGP latitude versus stratigraphic thickness at
Chani Khel 207
9 7 Plot of VGP latitude versus stratigraphic thickness at
Chichali and Khora Baroch 209
10 1 Locations of study sections in northern Pakistan 214
10 2 Ages of the study sections and approximate intervals in
which palaeosols were sampled for isotopic analysis 215
10 3 Profile of a palaeosol from about the 2 8 myr level at Mirpur 217
10 4 The stable carbon isotope contents of soil carbonate and
organic matter through time 221
10 5 The stable carbon and oxygen content of soil nodules, sandstone
nodules, and silty parent material in upper Siwalik beds 222
11 1 Location of study area in northern Pakistan 228
11 2 Detailed map of study area and thermoluminescence (TL)
dates of the deposit studied 230
12 1 Sui Dome in relation to major structural units in northwestern
Pakistan 238
12 2 Major subdivision of Siwalik Group within the Sui Dome
and location of sites mentioned in text 239
12 3 Distribution of teleseismic events 1914-15 and 1975-81 240
12 4 Diagram showing how undercutting gives rise to linear
topography 246
14 1 The modern environs of the Indus river and the Indus
synclinorium 267
14 2 Geomorphic development of the Punjab plains and the
Indus river plains 269
14 3 Prior and ancestral courses of the Indus river in the Holocene 271
14 4 Schematic longitudinal section of the Indus river and
associated landforms 278
14 5 A: the Jacobabad course and approximate coastline
~ 10,000-4000 yr BP; B: the Sindhu Nadi and Nara Nadi and
approximate coastline ~ 4000-2000 yr BC ( ~ 6000-4000 yr
BP); C: the Kandhkot course and approximate coastline
~ 2500-2000 yr BP 283
15 1 Location map 289
15 2 Tectonic zone map 291
15 3 Topographic map (A) and cross-valley profiles (B) of
the lower Indus river alluvial plain 292
15 4 Yearly water (A) and sediment (B) discharge for Sukkur and
Kotri stations 298
xiv
LIST OF FIGURES
15 5 Water surface profiles of the Indus river 301
15 6 Water surface profile (A) and profile slope (B) using valley
centre line distance in the place of channel distance 302
15 7 Channel maps based on four low-water surveys provided by
the Indus River Commission 305
15 8 Slope-discharge discriminant functions showing the
downstream change of the Indus river pattern sensitivity 307
15 9 Slope-sinuosity relationships of the Indus river 307
15 10 Cartoon showing the relationship of the Indus valley profile
and channel pattern to tectonic elements 310
15 11 Average, minimum and maximum flood depths for the
period 1973-85 311
15 12 Specific gauge height for 200,000 cfs ( ~ 5660 m V )
discharge showing the long-term trends of gauges near
barrages 313
15 13 Oscillation of the 200,000 cfs ( ~ 5660 mV) specific gauge
height about the trend reported in Table 15 2 for the stations
with the longest period of record 315
15 14 Oscillation of the 200,000 cfs ( ~ 5660 mV) specific gauge
height about the trend reported in Table 15 2 for the stations
with shorter gauge records 316
15 15 Sinuosity (channel distance/valley distance) for 10-20 km
sections of the Indus river for the period 1962-86, as
calculated from gauge-to-gauge river distances supplied by
the Indus River Commission 317
15 16 Change with time and distance downstream of the 200,000
cfs ( ~ 5660 mJs~ ) specific gauge height (A) and
sinuosity (B) 318
16 1 Location map of the Makran coastal region showing 25
terrace and platform areas 328
16 2 Tectonic setting of the Makran region 339
16 3 Geologic maps of the Makran coast of Iran (A) and
Pakistan (B) 340
16 4 Shelf-slope facies transitions from near shore to upper slope
within a single depositional cycle 342
16 5 Stratigraphic section of the Makran coast at Jiwani,
Pakistan 343
16 6 Stratigraphic section of Chah Bahar terrace 349
16 7 Landforms of the Konarak terrace region 351
16 8 Beris, Ras Fasteh and Gavater terraces in eastern Iran 352
16 9 Coastal changes at Ormara 353
16 10 Ras Tang terrace area in Iran 357
16 11 Results of MC dating of terrace deposits 359
16 12 Progressive development of marine terraces 360
xv
LIST OF FIGURES
17 1 The Makran coast of Pakistan 364
17 2 Archaeological sites in the Karachi region of Pakistan 366
17 3 Archaeological sites in the Las Bela valley 368
17 4 Distribution of summer and winter rainfall in southern
Pakistan 372
17 5 Tracks of major recorded Arabian Sea cyclones, 1847-1956 374
XVI
TABLES
1 1 Morphostructural zones of Pakistan, Afghanistan and part of
northwestern India 3
1 2 Criteria used on satellite imagery of the western Himalaya for
recognition of resolvable types of unusual differential or rapid
glacier movement followed by less rapid movement or retreat 18
1 3 Late Quaternary chronology in southern Pakistan and
northwestern India 21
2 1 Sedimentary budgets for each basin 66
2 2 Width of 2500 km long Himalayan slab required to account
for sediment budgets at different thicknesses 68
3 1 Summary precipitation data for the study areas 77
3 2 Selected rates of tectonic uplift for the study areas 78
3 3 The height of the equilibrium line in the northwest
Himalaya 85
3 4 Present and past equilibrium-line altitudes in the northwest
Himalaya 86
4 1 Site mean palaeomagnetic statistics for the four new sample
sites in the Bunthang sequence 103
5 1 Exhumation, denudation and uplift rates for selectioned areas
across the trans-Himalayan mountains 109
9 1 Directions of remnant magnetization for the four sites studied
in the Shinghar and Surghar ranges 211
10 1 Stable carbon and oxygen isotope analyses from upper Siwalik
Group and modern soils, northern Pakistan 219
11 1 Evidence of climatically related deposits in the Potwar area 229
13 1 Major characteristics of the Indus and its tributaries 253
13 2 Area affected as a result of 1988 floods 254
15 1 Location of gauges and barrages in km from the sea 296
15 2 Coefficients of nonparametric statistics of specific gauge
records for discharge of 5660 m3s~ 308
16 1 Structural and marine terraces and platforms of the Makran
coast of Pakistan and Iran 330
xvii
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genre | (DE-588)4143413-4 Aufsatzsammlung gnd-content |
genre_facet | Aufsatzsammlung |
geographic | Himalaja West (DE-588)4371079-7 gnd Pakistan (DE-588)4075812-6 gnd Himalaja (DE-588)4024923-2 gnd |
geographic_facet | Himalaja West Pakistan Himalaja |
id | DE-604.BV008849343 |
illustrated | Illustrated |
indexdate | 2024-07-09T17:26:00Z |
institution | BVB |
isbn | 0415066484 |
language | English |
oai_aleph_id | oai:aleph.bib-bvb.de:BVB01-005851176 |
oclc_num | 27727083 |
open_access_boolean | |
owner | DE-12 DE-824 DE-91 DE-BY-TUM DE-83 DE-11 DE-19 DE-BY-UBM DE-188 |
owner_facet | DE-12 DE-824 DE-91 DE-BY-TUM DE-83 DE-11 DE-19 DE-BY-UBM DE-188 |
physical | XXVII, 429 S. Ill., graph. Darst., Kt. |
publishDate | 1993 |
publishDateSearch | 1993 |
publishDateSort | 1993 |
publisher | Routledge |
record_format | marc |
spelling | Himalaya to the sea geology, geomorphology and the quaternary ed. by John F. Shroder 1. publ. London [u.a.] Routledge 1993 XXVII, 429 S. Ill., graph. Darst., Kt. txt rdacontent n rdamedia nc rdacarrier Geologie gtt Geomorfologie gtt Quartair gtt Geologie Geology Himalaya Mountains Region Geology Pakistan Geology, Stratigraphic Neogene Geology, Stratigraphic Quaternary Geomorphology Himalaya Mountains Region Geomorphology Pakistan Geologie (DE-588)4020227-6 gnd rswk-swf Geomorphologie (DE-588)4130684-3 gnd rswk-swf Himalaja West (DE-588)4371079-7 gnd rswk-swf Pakistan (DE-588)4075812-6 gnd rswk-swf Himalaja (DE-588)4024923-2 gnd rswk-swf (DE-588)4143413-4 Aufsatzsammlung gnd-content Himalaja (DE-588)4024923-2 g Geologie (DE-588)4020227-6 s DE-604 Geomorphologie (DE-588)4130684-3 s Pakistan (DE-588)4075812-6 g Himalaja West (DE-588)4371079-7 g Shroder, John F. Sonstige oth HEBIS Datenaustausch application/pdf http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=005851176&sequence=000002&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA Inhaltsverzeichnis |
spellingShingle | Himalaya to the sea geology, geomorphology and the quaternary Geologie gtt Geomorfologie gtt Quartair gtt Geologie Geology Himalaya Mountains Region Geology Pakistan Geology, Stratigraphic Neogene Geology, Stratigraphic Quaternary Geomorphology Himalaya Mountains Region Geomorphology Pakistan Geologie (DE-588)4020227-6 gnd Geomorphologie (DE-588)4130684-3 gnd |
subject_GND | (DE-588)4020227-6 (DE-588)4130684-3 (DE-588)4371079-7 (DE-588)4075812-6 (DE-588)4024923-2 (DE-588)4143413-4 |
title | Himalaya to the sea geology, geomorphology and the quaternary |
title_auth | Himalaya to the sea geology, geomorphology and the quaternary |
title_exact_search | Himalaya to the sea geology, geomorphology and the quaternary |
title_full | Himalaya to the sea geology, geomorphology and the quaternary ed. by John F. Shroder |
title_fullStr | Himalaya to the sea geology, geomorphology and the quaternary ed. by John F. Shroder |
title_full_unstemmed | Himalaya to the sea geology, geomorphology and the quaternary ed. by John F. Shroder |
title_short | Himalaya to the sea |
title_sort | himalaya to the sea geology geomorphology and the quaternary |
title_sub | geology, geomorphology and the quaternary |
topic | Geologie gtt Geomorfologie gtt Quartair gtt Geologie Geology Himalaya Mountains Region Geology Pakistan Geology, Stratigraphic Neogene Geology, Stratigraphic Quaternary Geomorphology Himalaya Mountains Region Geomorphology Pakistan Geologie (DE-588)4020227-6 gnd Geomorphologie (DE-588)4130684-3 gnd |
topic_facet | Geologie Geomorfologie Quartair Geology Himalaya Mountains Region Geology Pakistan Geology, Stratigraphic Neogene Geology, Stratigraphic Quaternary Geomorphology Himalaya Mountains Region Geomorphology Pakistan Geomorphologie Himalaja West Pakistan Himalaja Aufsatzsammlung |
url | http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=005851176&sequence=000002&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA |
work_keys_str_mv | AT shroderjohnf himalayatotheseageologygeomorphologyandthequaternary |